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        <Abstract>Il plan secturial Militar (PSM) è in instrument da planisaziun e da coordinaziun da la Confederaziun en il senn da l`art. 13 da la Lescha davart la planisaziun dal territori (LPT; CS 700). El serva a la garanzia territoriala sco er a la coordinaziun da las infrastructuras militaras e da las activitads cun las pretensiuns territorialas civilas e fixescha en moda lianta per las autoritads - en concordanza cun il concept da staziunament actual - las finamiras e las prescripziuns per las infrastructuras militaras ch`èn relevantas per il plan secturial. Pervia da las transfurmaziuns en connex cun la politica da segirezza e cun il militar sa midan permanentamain ils basegns da l`infrastructura e las pretensiuns territorialas da l`armada. Il PSM vegn perquai examinà ed adattà regularmain. Il PSM cumpiglia differentas categorias d`objects: plazzas d`armas, plazzas da tir, plazzas d`exercizi, plazzas aviaticas militaras, lieus logistics da l`armada, centers da recrutaziun, lieus da traversada e stabiliments spezials. Infrastructuras militaras pli pitschnas u talas ch`èn suttamessas a la Lescha davart la protecziun da stabiliments militars (CS 510.518) na figureschan betg en il PSM.</Abstract>
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        <Abstract>L`applicaziun web PROJEKTIL serva a la visualisaziun da:- donns da tir d`enfin ussa vi dals bostgs incl. donns consecutivs ch`èn vegnids chaschunads dal militar, sco er - plazzas da tir. Tras la visualisaziun sur l`internet vegn messa a disposiziun als schefexperts selvicultura in instrument effizient per sa far in maletg dals donns da tir d`enfin ussa e da las plazzas da tir. Quai cun la finamira da reducir donns futurs e pia pajaments d`indemnisaziuns ch`èn colliads cun quai (prevenziun).</Abstract>
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        <Abstract>La sumbriva dal reliev DHM25 deriva dal model digital da l`autezza DHM25. Ella permetta da visualisar il reliev da la Svizra e da l`exteriur vischin. La sumbriva dal reliev DHM25 è in maletg digital sumbrivà cun ina incidenza da la glisch calculada a l`acimut 315° (nord-vest) ed ad in angul da 45°. Il model digital da l`autezza DHM25 è ina matrix da l`autezza cun ina largezza da 25 m.</Abstract>
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        <Abstract>La rait triangulara sin il nivel da la mesiraziun naziunala (FINELTRA-MN) è vegnida terminada ils onns 1990 ed ha permess da transfurmar geodatas da la MN03 a la MN95 e viceversa cun in`exactadad da circa 1 decimeter. Ils ultims onns è questa rait triangulara vegnida rendida sistematicamain pli spessa tras ils chantuns. swisstopo l`ha unida l`onn 2006 ad in`unitad da datas cun la designaziun CHENyx06. Cun CHENyx06 pon geodatas vegnir transfurmadas cun in`exactadad d`en media 2 cm da la MN03 a la MN95 e viceversa. Ils puncts da chantun dals singuls trianguls èn uschenumnads puncts da sustegn per la transfurmaziun (PST). Quests puncts èn vegnids mesirads tant en il rom da referenza MN03 sco er MN95 en moda fitg precisa. Ils PST da la categoria 1 e 2 èn disponibels sur il servetsch da datas per ils puncts fixs u sur il portal federal da geodatas map.geo.admin.ch &gt; nivel dals puncts fixs planimetrics. Infurmaziuns davart ils auters PST èn disponiblas tar ils chantuns.</Abstract>
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      <Abstract>Model da geoid da la Svizra en la versiun da l`onn 2004 (CHGeo2004) en il sistem da referenza CH1903. El furma la surfatscha da referenza nulla (en media datiers dal livel mesaun da la mar) per determinar l`autezza e serva a transfurmar tranter autezzas ellipsoidalas ed autezzas ortometricas LHN95. Las autezzas da geoid èn registradas en in giatter regular dad 1 x 1 km e vegnan interpoladas cun agid da la metoda biquadrata. Il model è disponibel en differents sistems da referenza e formats.</Abstract>
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        <Abstract>Model da geoid da la Svizra en la versiun da l`onn 2004 (CHGeo2004) en il sistem da referenza CH1903. El furma la surfatscha da referenza nulla (en media datiers dal livel mesaun da la mar) per determinar l`autezza e serva a transfurmar tranter autezzas ellipsoidalas ed autezzas ortometricas LHN95. Las autezzas da geoid èn registradas en in giatter regular dad 1 x 1 km e vegnan interpoladas cun agid da la metoda biquadrata. Il model è disponibel en differents sistems da referenza e formats.</Abstract>
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      <Abstract>Model da geoid da la Svizra en la versiun da l`onn 2004 (CHGeo2004) en il sistem da referenza ETRS89. El furma la surfatscha da referenza nulla (en media datiers dal livel mesaun da la mar) per determinar l`autezza e serva a transfurmar tranter autezzas ellipsoidalas ed autezzas ortometricas LHN95. Las autezzas da geoid èn registradas en in giatter regular da 30 x 30 secundas e vegnan interpoladas cun agid da la metoda biquadrata. Il model è disponibel en differents sistems da referenza e formats.</Abstract>
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        <Abstract>Model da geoid da la Svizra en la versiun da l`onn 2004 (CHGeo2004) en il sistem da referenza ETRS89. El furma la surfatscha da referenza nulla (en media datiers dal livel mesaun da la mar) per determinar l`autezza e serva a transfurmar tranter autezzas ellipsoidalas ed autezzas ortometricas LHN95. Las autezzas da geoid èn registradas en in giatter regular da 30 x 30 secundas e vegnan interpoladas cun agid da la metoda biquadrata. Il model è disponibel en differents sistems da referenza e formats.</Abstract>
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        <Abstract>Il model descriva la media da la canera seismica spetgada tras influenzas antropogenas en nm/s en il champ da frequenza dad 1-40 Hz. Il model è deducì da datas da l`utilisaziun dal terren e da l`infrastructura dal traffic ed è vegnì calibrà a maun da passa 600 mesiraziuns da test seismologicas. (Kraft, T., A high-resolution and calibrated model of man-made seismic noise for Europe, 76. Dieta annuala da la DGG, Münster, 16 da mars 2016)</Abstract>
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        <Abstract>En ils funs ed en la crappa èn avant maun isotops instabils natirals da differents elements - per exempel uran, torium u calium - che produceschan ina radiaziun radioactiva, cur ch`els scrodan. Dals 30 fin 40 cm ils pli sisum dal terren deriva la gronda part da la radiaziun mesirada a la surfatscha. L`intensitad da la radiaziun terrestra vegn mesirada 1 meter sur il terren ed inditgada cun nanosieverts per ura (nSv/h). En Svizra chattan ins en spezial en las Alps crappa cun concentraziuns pli grondas d`uran, da torium e da calium. La charta da l`intensitad da la radiaziun terrestra sa basa sin differentas metodas da mesirar: Per l`ina vegn eruida la radioactivitad cun mesiraziuns gammaspectrometricas da provas da terren en il labor. Las activitads vegnan però er fatgas cun agid da mesiraziuns eroradiometricas e gammaspectrometricas al lieu. Perquai ch`ils puncts da mesiraziun èn repartids en moda eterogena sur la Svizra, vegnan las datas avant maun interpoladas ad ina rait da 2 x 2 kilometers.</Abstract>
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        <Abstract>La charta (GK500-LGM) represchenta l`extensiun la pli gronda dals glatschers en Svizra durant il zenit da l`ultim temp da glatsch avant circa 24`000 onns. Cun quella vegnan visualisads ils resultats ils pli actuals da la perscrutaziun indigena dal temp da glatsch en moda cartografica d`auta qualitad. La cumposiziun ed il luar dals glatschers expriman midadas ecologicas impurtantas chaschunadas dal clima en il passà geologic il pli giuven. - Dad &#39;Schlüchter, C. (compil.) 2009. Die Schweiz während des letzteiszeitlichen Maximums (LGM), 1:500`000. GeoKarten500, Bundesamt für Landestopografie swisstopo, Wabern.&#39;</Abstract>
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        <Abstract>A maun da perimeters da model dat l`unitad da datas `Models geologics 3D` ina survista dals models ch`existan gia e dals models ch`èn en elavuraziun. Ultra da quai vegnan dadas infurmaziuns da basa impurtantas davart ils models. Ils models èn vegnids elavurads da l`Uffizi federal da topografia swisstopo, d`universitads, da chantuns e d`interpresas privatas. Per infurmaziuns davart ils singuls models As drizzai per plaschair directamain al contact correspundent.</Abstract>
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        <Abstract>L`unitad da datas Profils GA25 (GA25_CS) è ina cumpilaziun dals profils publitgads en l`Atlas geologic 1:25 000. Ella mussa las lingias dals profils e cuntegna metadatas per mintga profil. L`onn d`ediziun inditgà correspunda a l`onn da publicaziun da las explicaziuns correspundentas. Ils profils che appartegnan a las lingias èn vegnids tagliads or da las tavlas dals profils e sche pussaivel vegnids arcunads individualmain sco PDF, cun l`entira legenda da la tavla e cun la scala da la tavla. Las legendas sa refereschan mintgamai a la tavla. En il singul profil na vegnan perquai betg adina mussads tut ils elements ch`èn cuntegnids en la legenda. En paucs cas n`han tavlas cun profils memia spess betg pudì vegnir dividids en singuls profils. En quests cas vegn mussada mintgamai l`entira tavla per pliras lingias da profil. LINK: &lt;a href=&#39;https://www.geocat.ch/geonetwork/srv/api/records/345d02a3-9628-46d7-9e57-e0ab1d9faf8a/attachments/GA25_Profile_Faktenblatt_DE_230113.pdf?approved=true&#39; target=&#39;_blank&#39;&gt;Faktenblatt&lt;/a&gt; LINK: &lt;a href=&#39;https://www.geocat.ch/geonetwork/srv/api/records/345d02a3-9628-46d7-9e57-e0ab1d9faf8a/attachments/GA25_Profile_Modellbeschreibung_DE_230113.pdf?approved=true&#39; target=&#39;_blank&#39;&gt;Modellbeschreibung&lt;/a&gt; LINK: &lt;a href=&#39;https://map.geo.admin.ch/?topic=geol&amp;lang=de&amp;bgLayer=ch.swisstopo.pixelkarte-grau&amp;layers=ch.swisstopo.geologie-geologischer_atlas&amp;catalogNodes=1787&#39; target=&#39;_blank&#39;&gt;map.geo.admin.ch - Geologischer Atlas GA25&lt;/a&gt; Exclusiun da la responsabladad: L`utilisadra u l`utilisader renconuscha, che las auturas ed ils auturs han fatg tut las stentas necessarias e pretendiblas per verifitgar las infurmaziuns en il model / en l`unitad da datas qua avant maun. I na dat nagina garanzia che las datas inditgadas èn correctas per in tschert punct dal sutterren. L`editur n`è en nagin cas responsabel per perditas u donns da gener material u immaterial che resultan tras l`access, tras l`utilisaziun da las infurmaziuns publitgadas, tras abus u tras disturbis tecnics.</Abstract>
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      <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa las lingias d`autezza da las isotermas da 100 °C ed las ruttadiras sin il medem nivel. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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        <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa las lingias d`autezza da las isotermas da 100 °C ed las ruttadiras sin il medem nivel. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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      <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa las lingias d`autezza da las isotermas da 150 °C ed las ruttadiras sin il medem nivel. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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        <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa las lingias d`autezza da las isotermas da 150 °C ed las ruttadiras sin il medem nivel. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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      <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa las lingias d`autezza da las isotermas da 60°C ed las ruttadiras sin il medem nivel. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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        <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa las lingias d`autezza da las isotermas da 60°C ed las ruttadiras sin il medem nivel. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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      <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa las temperaturas sisum il Muschelkalk sco er l`autezza da questa surfatscha e ses ruttadiras. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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        <Title>Temperaturas sisum il Muschelkalk</Title>
        <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa las temperaturas sisum il Muschelkalk sco er l`autezza da questa surfatscha e ses ruttadiras. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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      <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa las temperaturas sisum il Malm superiur sco er l`autezza da questa surfatscha e ses ruttadiras. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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        <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa las temperaturas sisum il Malm superiur sco er l`autezza da questa surfatscha e ses ruttadiras. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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      <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa las temperaturas sisum la Molassa marina superiura (OMM) sco er l`autezza da questa surfatscha e ses ruttadiras. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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        <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa las temperaturas sisum la Molassa marina superiura (OMM) sco er l`autezza da questa surfatscha e ses ruttadiras. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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      <Abstract>Questa charta mussa la posiziun da las datas d`entrada sco er il cunfin dal model da temperatura GeoMol15. Sco tala avess questa charta da vegnir duvrada en cumbinaziun cun las chartas da temperatura GeoMol15 appartegnentas, quai vul dir: &lt;ul&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperatur_top_omm&#39; target=&#39;_blank&#39;&gt;Temperaturas sisum la OMM&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperatur_top_omalm&#39; target=&#39;_blank&#39;&gt;Temperaturas sisum il Malm superiur&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperatur_top_muschelkalk&#39; target=&#39;_blank&#39;&gt;Temperaturas sisum il Muschelkalk&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturverteilung_500&#39; target=&#39;_blank&#39;&gt;Temperaturas en la profunditad da 500 m&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturverteilung_1000&#39; target=&#39;_blank&#39;&gt;Temperaturas en la profunditad da 1000 m&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturverteilung_1500&#39; target=&#39;_blank&#39;&gt;Temperaturas en la profunditad da 1500 m&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturverteilung_2000&#39; target=&#39;_blank&#39;&gt;Temperaturas en la profunditad da 2000 m&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturverteilung_3000&#39; target=&#39;_blank&#39;&gt;Temperaturas en la profunditad da 3000 m&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturverteilung_4000&#39; target=&#39;_blank&#39;&gt;Temperaturas en la profunditad da 4000 m&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-isotherme_60&#39; target=&#39;_blank&#39;&gt;Nivel isoterma da 60 °C&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-isotherme_100&#39; target=&#39;_blank&#39;&gt;Nivel isoterma da 100 °C&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-isotherme_150&#39; target=&#39;_blank&#39;&gt;Nivel isoterma da 150 °C&lt;/a&gt;&lt;/li&gt; &lt;/ul&gt;Las posiziuns da las datas d`entrada mussadas sin questa charta includan tant ils sondagis - dals quals in è in punct da sustegn - sco er il cunfin dal model da temperatura da la metoda FE (Geowatt AG, 2015). Ulteriuras indicaziuns stattan a disposiziun en la chascha d`infurmaziun (infobox) correspundenta ch`è attribuida a mintga charta da temperatura.</Abstract>
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        <Abstract>Questa charta mussa la posiziun da las datas d`entrada sco er il cunfin dal model da temperatura GeoMol15. Sco tala avess questa charta da vegnir duvrada en cumbinaziun cun las chartas da temperatura GeoMol15 appartegnentas, quai vul dir: &lt;ul&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperatur_top_omm&#39; target=&#39;_blank&#39;&gt;Temperaturas sisum la OMM&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperatur_top_omalm&#39; target=&#39;_blank&#39;&gt;Temperaturas sisum il Malm superiur&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperatur_top_muschelkalk&#39; target=&#39;_blank&#39;&gt;Temperaturas sisum il Muschelkalk&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturverteilung_500&#39; target=&#39;_blank&#39;&gt;Temperaturas en la profunditad da 500 m&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturverteilung_1000&#39; target=&#39;_blank&#39;&gt;Temperaturas en la profunditad da 1000 m&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturverteilung_1500&#39; target=&#39;_blank&#39;&gt;Temperaturas en la profunditad da 1500 m&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturverteilung_2000&#39; target=&#39;_blank&#39;&gt;Temperaturas en la profunditad da 2000 m&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturverteilung_3000&#39; target=&#39;_blank&#39;&gt;Temperaturas en la profunditad da 3000 m&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturverteilung_4000&#39; target=&#39;_blank&#39;&gt;Temperaturas en la profunditad da 4000 m&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-isotherme_60&#39; target=&#39;_blank&#39;&gt;Nivel isoterma da 60 °C&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-isotherme_100&#39; target=&#39;_blank&#39;&gt;Nivel isoterma da 100 °C&lt;/a&gt;&lt;/li&gt; &lt;li&gt;&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-isotherme_150&#39; target=&#39;_blank&#39;&gt;Nivel isoterma da 150 °C&lt;/a&gt;&lt;/li&gt; &lt;/ul&gt;Las posiziuns da las datas d`entrada mussadas sin questa charta includan tant ils sondagis - dals quals in è in punct da sustegn - sco er il cunfin dal model da temperatura da la metoda FE (Geowatt AG, 2015). Ulteriuras indicaziuns stattan a disposiziun en la chascha d`infurmaziun (infobox) correspundenta ch`è attribuida a mintga charta da temperatura.</Abstract>
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      <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutteren Questa charta mussa la distribuziun da la temperatura e la posiziun da las ruttadiras en ina profunditad da 1000m sut la surfatscha da la terra. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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        <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutteren Questa charta mussa la distribuziun da la temperatura e la posiziun da las ruttadiras en ina profunditad da 1000m sut la surfatscha da la terra. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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        <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa la distribuziun da la temperatura e la posiziun da las ruttadiras en ina profunditad da 1500 m sut la surfatscha da la terra. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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      <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa la distribuziun da la temperatura e la posiziun da las ruttadiras en ina profunditad da 2000 m sut la surfatscha da la terra. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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        <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa la distribuziun da la temperatura e la posiziun da las ruttadiras en ina profunditad da 2000 m sut la surfatscha da la terra. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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      <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa la distribuziun da la temperatura e la posiziun da las ruttadiras en ina profunditad da 3000 m sut la surfatscha da la terra. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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        <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa la distribuziun da la temperatura e la posiziun da las ruttadiras en ina profunditad da 3000 m sut la surfatscha da la terra. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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      <Abstract>In parameter impurtant per giuditgar il potenzial geotermic dal batschigl da molassa svizzer è la distribuziun da la temperatura el sutterren. Questa charta mussa la distribuziun da la temperatura e la posiziun da las ruttadiras en ina profunditad da 4000 m sut la surfatscha da la terra. Ella fa part d`ina seria da chartas che mussan la distribuziun da la temperatura sin surfatschas selecziunadas (represchentond orizonts marcaders seismics, profunditads constantas sut la surfatscha da la terra u isotermas). Las surfatschas d`orizont derivan dal model 3D geologic GeoMol15 e dal model da temperatura GeoMol15 che sa basa sin tal e che consista da cellas regularas d`ina grondezza da 1000x1000x100m. Quest model da temperatura en blocs è deducì d`in model da temperatura da la metoda FE (Geowatt AG, 2015) che sa basa oravant tut sin 31 profils da temperatura verticals e sin las surfatschas d`orizont da l`&lt;a href=&#39;https://www.geologieportal.ch/de/themen/grundlagen-der-geologie/geophysik/seismischer-atlas.html&#39; target=&#39;_blank&#39;&gt;Atlas seismic dal batschigl da molassa svizzer (2012)&lt;/a&gt;. La metoda da modellament da las temperaturas FE (elements finits) lavura mo cun il fluss da chalur conductiv. Ella na resguarda betg il fluss da chalur convectiv. Il model GeoMol15 ed il model da temperatura appartegnent stattan a disposiziun online sut &lt;a href=&#39;https://viewer.geomol.ch/webgui/gui2.php&#39; target=&#39;_blank&#39;&gt;GeoMol-Viewer&lt;/a&gt;. Guardar er la charta appartegnenta `&lt;a href=&#39;https://map.geo.admin.ch/?layers=ch.swisstopo.geologie-geomol-temperaturmodell_eingangsdaten&#39; target=&#39;_blank&#39;&gt;Model da temperatur - datas&lt;/a&gt;` sin map.geo.admin.ch.</Abstract>
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      <Abstract>La rait da mesiraziun dals glatschers svizzers (GLAMOS) ha l`intent da documentar a lunga vista las midadas dals glatschers en Svizra. I vegnan registradas sistematicamain datas dal svilup da la surfatscha, dal volumen, ma er da l`accumulaziun da naiv e dal regress dals glatschers sco er dals moviments da flussiun dals glatschers e da las temperaturas dal glatsch. Questas infurmaziuns èn impurtantas per chapir l`effect reciproc tranter ils glatschers ed il clima. Ellas servan a giuditgar las resursas d`aua, ils privels da la natira e l`augment futur dal nivel da la mar. Inventaris dals glatschers cumpiglian las conturas, las surfatschas ed ulteriuras caracteristicas da tut ils glatschers d`in territori en in tschert mument. Per las Alps svizras datti tals inventaris cumplets per las periodas 1850 (reconstruids posteriuramain), 1973, 2010 e 2016 (fatgs sin basa da fotografias ord l`aria).</Abstract>
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        <Abstract>La Charta topografica da la Svizra 1:100`000 (Charta Dufour) è l`emprima ovra cartografica uffiziala che cuvra l`entira Svizra. Ella è vegnida publitgada tranter 1845 e 1865 ed è vegnida actualisada fin l`onn 1939. L`unitad da datas `Divisiun Charta Dufour` mussa il perimeter, il numer ed il num da mintga fegl. Ils fegls stampads cun las parts extendidas vegnan preschentads cun surfatschas in pau pli grondas ch`ils fegls da standard. Il frontispizi e las chartas Fort de l`Ecluse, Rheineck e Bergamo vegnan preschentads ensemen cun ina charta vischina.</Abstract>
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      <Abstract>A partir da l`onn 2020 vegn SWISSIMAGE 10 cm ad esser disponibel per tut la surfatscha da la Svizra e dal Liechtenstein. Ultra da quai cumpiglia SWISSIMAGE ina pitschna part da las regiuns cunfinantas vischinas. SWISSIMAGE 10 cm vegn producì en quadrels da mintgamai 1 km2. La numeraziun dals quadrels correspunda a las coordinatas kilometricas dal chantun sidvest d`in quadrel. Ultra da la qualitad geometrica e radiometrica è la data dal maletg fatg ord l`aria da gronda impurtanza per pudair duvrar optimalmain in`ortofoto. L`onn dal sgol vegn perquai inditgà per mintga quadrel. En las regiuns perifericas dals blocs da sgol poi capitar ch`ils quadrels cumpiglian maletgs da differents onns. Quests quadrels han perquai pixels da differents onns da sgol. Attribuì vegn mintgamai l`onn cun la gronda part dals pixels (passa 75 % da tut ils pixels).</Abstract>
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        <Abstract>A partir da l`onn 2020 vegn SWISSIMAGE 10 cm ad esser disponibel per tut la surfatscha da la Svizra e dal Liechtenstein. Ultra da quai cumpiglia SWISSIMAGE ina pitschna part da las regiuns cunfinantas vischinas. SWISSIMAGE 10 cm vegn producì en quadrels da mintgamai 1 km2. La numeraziun dals quadrels correspunda a las coordinatas kilometricas dal chantun sidvest d`in quadrel. Ultra da la qualitad geometrica e radiometrica è la data dal maletg fatg ord l`aria da gronda impurtanza per pudair duvrar optimalmain in`ortofoto. L`onn dal sgol vegn perquai inditgà per mintga quadrel. En las regiuns perifericas dals blocs da sgol poi capitar ch`ils quadrels cumpiglian maletgs da differents onns. Quests quadrels han perquai pixels da differents onns da sgol. Attribuì vegn mintgamai l`onn cun la gronda part dals pixels (passa 75 % da tut ils pixels).</Abstract>
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        <Abstract>Preschentaziun deducida dal model digital da l`autezza swissALTI3D e d`elements dal model cartografic digital, cun la quala po vegnir preschentà il reliev da la Svizra e dal Principadi da Liechtenstein. Questa varianta è vegnida fatga per la `charta da basa ligera` (light base map). Ella cumbinescha elements da la charta naziunala 1:25 000 (il reliev ch`è oriundamain vegnì fatg a maun, il tun mellen dal sulegl, las preschentaziuns da la cuntrada spelm, glera e glatscher) e dal model da l`autezza swissALTI3D. Il cuntegn variescha tut tenor il stgalim da zoom.</Abstract>
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        <Abstract>La collecziun da fotografias da swisstopo cumpiglia pliras tschientmill fotos aviaticas analogas (en colur, infrarot u alv e nair). Quellas vegnan represchentadas sco coordinatas dal center da la maletg, da las zonas ch`ellas cuvran (footprint), sco er cun lur metadatas (cun ils elements d`orientaziun correspundents sche disponibels). Sche ellas èn gia digitalisadas, pon las maletgs vegnir telechargiadas e visualisadas en resoluziun totala. Las scans ch`anc mancan vegnan successivamain integradas ed alura messas a disposiziun directamain.En il rom dal program Sanasilva per registrar il stadi da sanadad dals guauds èn vegnidas gravadas lingias directamain sin intginas fotografias aerias originalas. Tenor l`incumbensader da lez temp vegnivan questas marcaziuns duvradas durant l`evaluaziun per distinguer tranter differentas populaziuns d`arbais, pia populaziuns da la medema vegliadetgna e/u cun la medema cumposiziun da spezias.</Abstract>
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        <Abstract>La collecziun da fotografias da swisstopo cumpiglia pliras tschientmill fotos aviaticas analogas (en colur, infrarot u alv e nair). Quellas vegnan represchentadas sco coordinatas dal center da la maletg, da las zonas ch`ellas cuvran (footprint), sco er cun lur metadatas (cun ils elements d`orientaziun correspundents sche disponibels). Sche ellas èn gia digitalisadas, pon las maletgs vegnir telechargiadas e visualisadas en resoluziun totala. Las scans ch`anc mancan vegnan successivamain integradas ed alura messas a disposiziun directamain.</Abstract>
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        <Abstract>La Charta naziunala 1:100`000 è ina charta topografica surregiunala da la Svizra. Il perimeter da la charta è dividì en 23 fegls singuls. Per tschertas regiuns existan cumposiziuns. La Charta naziunala 1:100`000 è disponibla en furma analoga (charta da palpiri) e digitala (Swiss Map Raster). L`actualisaziun vegn fatga tenor secturs. Die verschiedenen Nachführungsstände zeigt der Layer &#39;&lt;a href=&#39;https://map.geo.admin.ch/?lang=rm&amp;topic=ech&amp;bgLayer=ch.swisstopo.pixelkarte-farbe&amp;layers=ch.swisstopo.pixelkarte-pk100.metadata&#39; target=&#39;_blank&#39;&gt;Div. Charta naziunala 100 Raster&lt;/a&gt;&#39;.</Abstract>
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        <Abstract>La Charta naziunala 1:200`000 è ina charta da survista topografica da la Svizra. Il perimeter da la charta è dividì en 4 (charta da palpiri) u 16 (Swiss Map Raster) fegls singuls. La Charta naziunala 1:200`000 è disponibla en furma analoga (charta da palpiri) e digitala (Swiss Map Raster). L`actualisaziun vegn fatga tenor secturs. Die verschiedenen Nachführungsstände zeigt der Layer &#39;&lt;a href=&#39; https://map.geo.admin.ch/?lang=rm&amp;topic=ech&amp;bgLayer=ch.swisstopo.pixelkarte-farbe&amp;layers=ch.swisstopo.pixelkarte-pk200.metadata&#39; target=&#39;_blank&#39;&gt;Div. Charta naziunala 200 Raster&lt;/a&gt;&#39;.</Abstract>
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        <Abstract>La Charta naziunala 1:25`000 è ina charta topografica da la Svizra cun ina preschentaziun fitg detagliada dal traffic, dals abitadis, dal territori e da la vegetaziun. L`actualisaziun vegn fatga tenor secturs. La Charta naziunala 1:25`000 è disponibla en furma analoga (charta da palpiri) e digitala (Swiss Map Raster, Swiss Map Vector). Im Kartenviewer des Bundes wird standardmässig der aktuellste Stand der Karte angezeigt. Mit der `Zeitreise`-Funktion lassen sich alle verfügbaren Datenstände seit 1952 anzeigen. Die detaillierten Datenstände zeigt der Layer &#39;&lt;a href=&#39;https://map.geo.admin.ch/?lang=rm&amp;topic=ech&amp;bgLayer=ch.swisstopo.pixelkarte-farbe&amp;layers=ch.swisstopo.pixelkarte-pk25.metadata&#39; target=&#39;_blank&#39;&gt;Div. Charta naziunala 25 Raster&lt;/a&gt;&#39;.</Abstract>
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        <Abstract>La Charta naziunala 1:50`000 è ina charta topografica da la Svizra cun ina preschentaziun detagliada dal traffic, dals abitadis, dal territori, da las auas e da la vegetaziun. Il perimeter da la charta è dividì en 78 fegls singuls. Per tschertas regiuns existan cumposiziuns. La Charta naziunala 1:50`000 è disponibla en furma analoga (charta da palpiri) e digitala (Swiss Map Raster). L`actualisaziun vegn fatga tenor secturs. Die verschiedenen Nachführungsstände zeigt der Layer &#39;&lt;a href=&#39;https://map.geo.admin.ch/?lang=rm&amp;topic=ech&amp;bgLayer=ch.swisstopo.pixelkarte-farbe&amp;layers=ch.swisstopo.pixelkarte-pk50.metadata&#39; target=&#39;_blank&#39;&gt;Div. Charta naziunala 50 Raster&lt;/a&gt;&#39;.</Abstract>
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        <Abstract>L`unitad da datas `Divisiun Swiss Map Raster 100` mussa il perimeter, il numer ed il num da mintga fegl. Il perimeter correspunda ad in fegl da standard d`ina charta stampada. Las parts extendidas cuntegnidas sin ils fegls da la charta stampada (p.ex. part ost dal fegl 39 Flüelapass) vegnan preschentadas sin fegls supplementars da standard, er sche quels cuntegnan mo infurmaziuns per tschertas parts.publicaziun.La Swiss Map Raster vegn furnida sco datoteca georeferenziada en format TIF (format da raster). Las infurmaziuns da la charta èn divididas tenor stresas da colur, dentant betg tenor elements tematics. Las chartas da pixels stattan a disposiziun sco cumbinaziuns da colurs (508 dpi) u sco fegls separads tenor colurs (datas binaras 508 dpi), e pon vegnir retratgas sco fegls singuls u sco extract individualisà.</Abstract>
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      <Abstract>L`unitad da datas `Divisiun Swiss Map Raster 50` mussa il perimeter, il numer ed il num da mintga fegl. Il perimeter correspunda ad in fegl da standard d`ina charta stampada. Las parts extendidas cuntegnidas sin ils fegls da la charta stampada (p.ex. part sid dal fegl 270 Genève) vegnan preschentadas sin fegls supplementars da standard, er sche quels cuntegnan mo infurmaziuns per tschertas parts.La Swiss Map Raster vegn furnida sco datoteca georeferenziada en format TIF (format da raster). Las Las chartas da pixels stattan a disposiziun sco cumbinaziuns da colurs (508 dpi) u sco layers tenor colurs separadas (datas binaras 508 dpi). Ellas pon vegnir retratgas sco fegls singuls u sco extract individualisà.</Abstract>
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        <Abstract>L`unitad da datas `Divisiun Swiss Map Raster 50` mussa il perimeter, il numer ed il num da mintga fegl. Il perimeter correspunda ad in fegl da standard d`ina charta stampada. Las parts extendidas cuntegnidas sin ils fegls da la charta stampada (p.ex. part sid dal fegl 270 Genève) vegnan preschentadas sin fegls supplementars da standard, er sche quels cuntegnan mo infurmaziuns per tschertas parts.La Swiss Map Raster vegn furnida sco datoteca georeferenziada en format TIF (format da raster). Las Las chartas da pixels stattan a disposiziun sco cumbinaziuns da colurs (508 dpi) u sco layers tenor colurs separadas (datas binaras 508 dpi). Ellas pon vegnir retratgas sco fegls singuls u sco extract individualisà.</Abstract>
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      <Abstract>Il mosaic d`ortofotos SWISSIMAGE è ina cumposiziun da fotografias ord l`aria analogas scannadas e digitalas, da colur u alv/nair. In`ortofoto è in maletg ord l`aria, sin il qual las influenzas da l`inclinaziun da la camera e dal reliev da la cuntrada èn neutralisadas. Sco standard vegn mussà il stadi actual dal product SWISSIMAGE. Cun la visualisaziun istorica da las datas, che vegn numnada `viadi en il temp`, sa lascha la transfurmaziun da la cuntrada da 1926 fin oz pertschaiver en moda interactiva a maun da questas fotografias.</Abstract>
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        <Title>SWISSIMAGE Viadi en il temp</Title>
        <Abstract>Il mosaic d`ortofotos SWISSIMAGE è ina cumposiziun da fotografias ord l`aria analogas scannadas e digitalas, da colur u alv/nair. In`ortofoto è in maletg ord l`aria, sin il qual las influenzas da l`inclinaziun da la camera e dal reliev da la cuntrada èn neutralisadas. Sco standard vegn mussà il stadi actual dal product SWISSIMAGE. Cun la visualisaziun istorica da las datas, che vegn numnada `viadi en il temp`, sa lascha la transfurmaziun da la cuntrada da 1926 fin oz pertschaiver en moda interactiva a maun da questas fotografias.</Abstract>
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        <Abstract>Il mosaic d`ortofoto SWISSIMAGE HIST 1946 è ina cumposiziun da maletgs ord l`aria en alv e nair da l`onn 1946 (`sursgulada americana`) da tut la Svizra cun ina dissoluziun al fund dad 1 m. In`ortofoto è in maletg ord l`aria, tar il qual las influenzas da l`inclinaziun da la camera e dal reliev da la cuntrada èn neutralisadas.</Abstract>
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        <Abstract>swissNAMES3D è la collecziun la pli cumpletta da nums geografics da la Svizra e dal principadi da Liechtenstein. swissNAMES3D cumpiglia sur 437`000 inscripziuns georeferenziadas ch`èn repartidas en differentas categorias. L`unitad da datas remplazza a partir da l`onn 2015 il product SwissNames che sa basa sin ils nums da las ovras da la Charta naziunala e ch`è vegnì actualisà fin l`onn 2008. La preschentaziun dals nums geografics en il geoportal da la Confederaziun correspunda ad ina selecziun or da swissNAMES3D ch`èn accordads al stgalim da zoom tschernì.</Abstract>
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      <Abstract>swissSURFACE3D beschreibt die Oberfläche der Schweiz mit allen natürlichen und künstlichen Elementen in Form einer klassifizierten Punktwolke. Die mit einem airborne LiDAR erhobenen Daten zeichnen sich durch eine hohe Punktdichte und Genauigkeit aus. swissSURFACE3D wird in Kacheln von jeweils 1 km2 produziert. Die Kachelnummerierung entspricht den Kilometerkoordinaten des südwestlichen Eckpunkts einer Kachel.</Abstract>
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        <Abstract>swissSURFACE3D beschreibt die Oberfläche der Schweiz mit allen natürlichen und künstlichen Elementen in Form einer klassifizierten Punktwolke. Die mit einem airborne LiDAR erhobenen Daten zeichnen sich durch eine hohe Punktdichte und Genauigkeit aus. swissSURFACE3D wird in Kacheln von jeweils 1 km2 produziert. Die Kachelnummerierung entspricht den Kilometerkoordinaten des südwestlichen Eckpunkts einer Kachel.</Abstract>
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        <Title>swissSURFACE3D Raster reliev multidirecziunal</Title>
        <Abstract>La sumbriva dal reliev deriva dal model digital da l`autezza dal raster swissSURFACE3D. Ella permetta da visualisar il reliev da la Svizra e dal Principadi da Liechtenstein. La sumbriva dal reliev è in maletg digital sumbrivà cun ina u pliras incidenzas da la glisch calculadas. Per represchentar la sumbriva dal reliev qua avant maun dal raster swissSURFACE3D èn vegnidas cumbinadas sis differentas posiziuns dal sulegl. La posiziun dal sulegl mesauna sa chatta en il nordvest.</Abstract>
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        <Abstract>La sumbriva dal reliev deriva dal model digital da l`autezza dal raster swissSURFACE3D. Ella permetta da visualisar il reliev da la Svizra e dal Principadi da Liechtenstein. La sumbriva dal reliev è in maletg digital sumbrivà cun ina u pliras incidenzas da la glisch calculadas. Per represchentar la sumbriva dal reliev monodirecziunala dal raster swissSURFACE3D èsi vegnì calculà cun ina posiziun dal sulegl da nordvest.</Abstract>
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        <Abstract>swissTLM3D Viafier cuntegna las axas dals binaris da las viafiers a binaris normals ed a binaris stretgs sco e da las viafiers pitschnas. En cas da stabiliments cun plirs binaris u en zonas da staziun èn adina registrads tut ils binaris. swissTLM3D Viafier è ina part integrala da l`unitad da datas swissTLM3D. Cun sia auta precisiun e cun l`integraziun da la terza dimensiun è swissTLM3D l`unitad da datas vectorialas en 3D la pli cumplessiva da la Svizra.</Abstract>
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      <Abstract>swissTLM3D Rait d`auas cuntegna ils curs d`aua e las conturas dals lais da la Svizra e dal Principadi da Liechtenstein. Ella è ina part integrala da l`unitad da datas swissTLM3D. Cun sia auta precisiun e cun l`integraziun da la terza dimensiun è swissTLM3D l`unitad da datas vectorialas en 3D la pli cumplessiva da la Svizra.</Abstract>
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        <Abstract>swissTLM3D Rait d`auas cuntegna ils curs d`aua e las conturas dals lais da la Svizra e dal Principadi da Liechtenstein. Ella è ina part integrala da l`unitad da datas swissTLM3D. Cun sia auta precisiun e cun l`integraziun da la terza dimensiun è swissTLM3D l`unitad da datas vectorialas en 3D la pli cumplessiva da la Svizra.</Abstract>
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        <Abstract>swissTLM-Map è ina charta generada dal tuttafatg automaticamain che porscha ina cumplettaziun a las chartas naziunalas per las scalas 1:5000 fin ca. 1:10`000. SwissTLM-Map sa basa sin las unitads da datas dal model topografic da la cuntrada swissTLM3D ed è cumplettà cun las lingias da l`autezza sur mar e cun ina sumbriva dal reliev che deriva dal model d`autezza swissALTI3D.</Abstract>
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        <Abstract>swissTLM3D Auters transports cuntegna differents geners da telefericas sco er auters sistems da transport mecanics. Ella è ina part integrala da l`unitad da datas swissTLM3D. Cun sia auta precisiun e cun l`integraziun da la terza dimensiun è swissTLM3D l`unitad da datas vectorialas en 3D la pli cumplessiva da la Svizra. En il geoportal da la Confederaziun vegnan ils objects dad &#39;Auters transports&#39; preschentads progressivamain, tut tenor il stgalim da zoom tschernì.</Abstract>
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      <Abstract>Il topic Hydrography cuntegna ils differents elements da las auas. El consista da 6 feature classes e d`ina tabella. Las lingias da &#39;FlowingWater&#39; e da &#39;StagnantWater&#39; ed ils puncts da &#39;GWK_FW_Node&#39; èn colliads topologicamain in cun l`auter tenor ina structura d`artgs e nufs, en la quala ils artgs (lingias) èn liads in cun l`auter tras nufs (puncts). Mintga artg ha pia exactamain dus nufs a sias fins. Ils artgs ed ils nufs furman ensemen ina rait geometrica. En collavuraziun cun l`Uffizi federal d`ambient (UFAM) èn ils nufs ed ils artgs en Svizra vegnids structurads ed adressads tenor GEWISS (sistem d`infurmaziun svizzer da las auas). Per quest intent èn vegnids introducids ils uschenumnads attributs GEWISS. Ina feature class che cuntegna infurmaziuns davart las cascadas, las sclusas ed ulteriurs objects è integrada en quest topic.</Abstract>
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        <Abstract>Puncts da mesiraziun furman la basa da tut las datas che sa refereschan al territori. Quests puncts fixs (puncts fixs planimetrics (PFP) e puncts fixs altimetrics (PFA2)) vegnan duvrads per tut las lavurs tecnicas che basegnan ina mesiraziun fidada ed exacta. In punct fix altimetric è in punct ch`è designà permanentamain cun in bullun, dal qual ins enconuscha l`autezza. Ils puncts fixs altimetrics da las categorias 2 (PFA2) servan a render pli spessa la rait da puncts e furman la basa per la mesiraziun uffiziala. Ils chantuns èn cumpetents per ils puncts fixs da la categoria 2. Las datas sa basan sin il model dal servetsch da datas per ils puncts fixs 2.0 da la Conferenza dals posts chantunals da geoinfurmaziun e cataster (model da datas KGKCGC_FDPS2_V1_1; versiun 1.1).</Abstract>
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        <Abstract>Puncts da mesiraziun furman la basa da tut las datas che sa refereschan al territori. Ils uschenumnads puncts fixs vegnan duvrads per tut las lavurs tecnicas che basegnan ina mesiraziun fidada ed exacta. In punct fix planimetric è in punct ch`è designà permanentamain cun in crap u cun in bullun (per part en in tumbin), dal qual ins enconuscha las coordinatas ed eventualmain l`autezza. La mesiraziun naziunala (swisstopo) è responsabla per ils puncts fixs planimetrics da la categoria 1 (PFP1). I dat differents tips: * Ils puncts fixs planimetrics da la categoria 1 (PFP1) furman il rom da referenza planimetric per tut las lavurs da mesiraziun en Svizra. Las coordinatas da la MN03 dals puncts fixs planimetrics istorics èn vegnidas determinadas cun agid da la triangulaziun il cumenzament dal 20avel tschientaner. * Ils puncts da sustegn per la transfurmaziun (PST1) èn puncts fixs planimetrics cun coordinatas exactas tant en il rom da referenza MN03 sco er MN95. * Ils puncts EUREF èn puncts fixs planimetrics da la rait da referenza da GNSS europeica EUREF (European Reference Frame). * Ils puncts da la MN95 èn puncts fixs planimetrics che furman la basa per il nov rom da referenza MN95. Las coordinatas da quests puncts èn vegnidas determinadas en moda fitg exacta cun agid da GNSS. Cunquai ch`in punct fix planimetric po vegnir attribuì a plirs tips, èsi pussaivel ch`ils simbols èn surpostads sin la charta.</Abstract>
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        <Abstract>La charta (GK500-LGM) represchenta l`extensiun la pli gronda dals glatschers en Svizra durant il zenit da l`ultim temp da glatsch avant circa 24`000 onns. Cun quella vegnan visualisads ils resultats ils pli actuals da la perscrutaziun indigena dal temp da glatsch en moda cartografica d`auta qualitad. La cumposiziun ed il luar dals glatschers expriman midadas ecologicas impurtantas chaschunadas dal clima en il passà geologic il pli giuven. - Dad &#39;Schlüchter, C. (compil.) 2009. Die Schweiz während des letzteiszeitlichen Maximums (LGM), 1:500`000. GeoKarten500, Bundesamt für Landestopografie swisstopo, Wabern.&#39;</Abstract>
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        <Abstract>La gravitad dependa dal lieu dal punct da mesiraziun e da la distribuziun da la massa en il sutterren. Anomalias da Bouguer numnan ins la differenza tranter la gravitad ch`è vegnida mesirada en in punct fixà sin la surfatscha da la terra e la valur da la gravitad calculada en il medem punct per in model terrester ideal cun crusta da terra omogena. Las anomalias da Bouguer èn calculadas cun agid da la furmla internaziunala da gravitad da l`onn 1967. L`influenza da la topografia è vegnida resguardada cun ina densitad constanta da 2670 kg/m3 fin ad ina distanza da 167 km (zona O2 tenor Hayford). La charta mussa d`ina vart las anomalias regiunalas negativas da la gravitad per lung da las Alps e da l`autra vart l`anomalia positiva da la zona Sesia-Finero, la quala signifitga in surpli da massa a l`intern da la terra. - Dad E. KLINGELE &amp; R. OLIVIER, 1979 - Nova ediziun R. OLIVIER, B. DUMONT &amp; E. KLINGELE, 2008</Abstract>
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        <Abstract>Utilisond l`ipotesa da Pratt u Airy po vegnir deducida l`anomalia isostatica. Questa anomalia correspunda a la divergenza da la crusta statica flottanta en il mantè superiur da la terra. La divergenza resguarda la structura da ragisch sut la crusta da la terra (chadaina da muntognas), la furma da la structura da ragisch na vegn però betg adina definida cleramain. Per la charta èn vegnidas duvradas l`ipotesa dad Airy-Heiskanen e las suandantas densitads: mantè da la terra = 3,31 g/cm3, crusta da la terra sut l`ellipsoid = 2,81 g/cm3, crusta da la terra sur l`ellipsoid = 2,67 g/cm3. - Dad E. KLINGELE, 1979.</Abstract>
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        <Abstract>La magnetisaziun totala da la crappa sa cumpona da la magnetisaziun inducida che vegn effectuada dal champ magnetic da la terra e da la magnetisaziun remanenta che la crappa ha obtegnì cura ch`ella è vegnida furmada. Divergenzas regiunalas u localas dal champ geomagnetic d`in model global, uschenumnadas anomalias, vegnan mesiradas or da l`aviun. Questas anomalias pon permetter l`identificaziun da las structuras geologicas e tectonicas e la preschientscha da concentraziuns da minerals. La charta eromagnetica speziala mussa l`intensitad totala dal champ magnetic (Epoca 1980.5) ch`è vegnida mesirada or d`ina autezza da sgol da 1829 m s.m. - Charta da palpiri: champ total, E. KLINGELE, 1982. - Charta vectoriala: versiun online, anomalias residualas eromagneticas (subtracziun da tendenzas regiunalas), E. KLINGELE, 2009.</Abstract>
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        <Abstract>La magnetisaziun totala da la crappa sa cumpona da la magnetisaziun inducida che vegn effectuada dal champ magnetic da la terra e da la magnetisaziun remanenta che la crappa ha obtegnì cura ch`ella è vegnida furmada. Divergenzas regiunalas u localas dal champ geomagnetic d`in model global, uschenumnadas anomalias, vegnan mesiradas or da l`aviun. Questas anomalias pon permetter l`identificaziun da las structuras geologicas e tectonicas e la preschientscha da concentraziuns da minerals. La charta eromagnetica da la Svizra mussa l`intensitad totala dal champ magnetic (Epoca 1981.5) ch`è vegnida mesirada or d`ina autezza da sgol da 5000 m s.m. - Charta da palpiri: champ total, E. KLINGELE, 1982. - Charta vectoriala: versiun online, anomalias residualas eromagneticas (subtracziun da tendenzas regiunalas), E. KLINGELE, 2009.</Abstract>
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        <Abstract>Las chartas geomagneticas resultan da las mesiraziuns da l`intensitad totala, da la declinaziun e da l`inclinaziun. La declinaziun exprima l`angul tranter il nord magnetic ed il nord geografic. Damai ch`il champ magnetic da la terra sa mida cun il temp, sa refereschan las indicaziuns da questas chartas adina ad ina tscherta perioda da temp. Las valurs pon vegnir adattadas cun agid da furmlas da correctura, da las qualas ils coeffizients èn vegnids calculads en experiments. - Charta da palpiri: G. FISCHER &amp; P.-A. SCHNEGG, 1979 (text explicativ sin la vart davos da la charta). - Charta vectoriala: 2001.</Abstract>
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        <Abstract>Las chartas geomagneticas resultan da las mesiraziuns da l`intensitad totala, da la declinaziun e da l`inclinaziun. L`inclinaziun è la pendenza da la direcziun dal champ magnetic vers l`orizont. Damai ch`il champ magnetic da la terra sa mida cun il temp, sa refereschan las indicaziuns da questas chartas adina ad ina tscherta perioda da temp. Las valurs pon vegnir adattadas cun agid da furmlas da correctura, da las qualas ils coeffizients èn vegnids calculads en experiments. - Charta da palpiri: G. FISCHER &amp; P.-A. SCHNEGG, 1979 (text explicativ sin la vart davos da la charta). - Charta vectoriala: 2001.</Abstract>
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        <Abstract>Las chartas geomagneticas resultan da las mesiraziuns da l`intensitad totala, da la declinaziun e da l`inclinaziun. Il champ geomagnetic vegn definì cun agid d`in vectur che vegn preschentà tras sia direcziun e sia intensitad (nT). Damai ch`il champ magnetic da la terra sa mida cun il temp, sa refereschan las indicaziuns da questas chartas adina ad ina tscherta perioda da temp. Las valurs pon vegnir adattadas cun agid da furmlas da correctura, da las qualas ils coeffizients èn vegnids calculads en experiments. - Charta da palpiri: G. FISCHER &amp; P.-A. SCHNEGG, 1979 (text explicativ sin la vart davos da la charta). - Charta vectoriala: 2001.</Abstract>
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        <Abstract>L`Uffizi federal d`ambient UFAM è il post spezialisà dal Servetsch geologic naziunal ch`è cumpetent per l`idrogeologia. La Charta idrogeologica 1:500`000 è integrada en la seria da las GeoChartas (GK500) e sa cumpona da dus fegls. L`emprim (GK500-Hydro) preschenta las differentas resursas d`aua sutterrana da la Svizra e lur productivitad, il segund (GK500-Hydro_Vul) la vulnerabilitad da las resursas d`aua sutterrana areguard eventualas periclitaziuns tras substanzas nuschaivlas. L`emprim fegl mussa ultra da quai il gener da las resursas d`aua sutterrana (crap carstic, crappa cun sfessas e crappa lucca), las tschiffadas las pli impurtantas da funtauna e d`aua sutterrana sco er indicaziuns idrodinamicas areguard ils territoris d`infiltraziun e d`exfiltraziun. Oriundamain èn ils dus fegls vegnids edids sco tavlas 8.6 ed 8.7 da l`Atlas idrologic da la Svizra HADES (UFAM, 2004 e 2007).</Abstract>
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        <Abstract>L`Uffizi federal d`ambient UFAM è il post spezialisà dal Servetsch geologic naziunal ch`è cumpetent per l`idrogeologia. La Charta idrogeologica 1:500`000 è integrada en la seria da las GeoChartas (GK500) e sa cumpona da dus fegls. L`emprim (GK500-Hydro) preschenta las differentas resursas d`aua sutterrana da la Svizra e lur productivitad, il segund (GK500-Hydro_Vul) la vulnerabilitad da las resursas d`aua sutterrana areguard eventualas periclitaziuns tras substanzas nuschaivlas. Il princip da la vulnerabilitad è in element impurtant da la protecziun preventiva da l`aua sutterrana. Oriundamain èn ils dus fegls vegnids edids sco tavlas 8.6 ed 8.7 da l`Atlas idrologic da la Svizra HADES (UFAM, 2004 e 2007).</Abstract>
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      <Abstract>swissBOUNDARIES3D cuntegna las unitads administrativas ed ils cunfins da la Svizra e dal Principadi da Liechtenstein en furma vectoriala. Il product sa basa sin in model da datas optimà per la Svizra ed è accordà cun las datas da l`Uffizi federal da statistica. swissBOUNDARIES3D remplazza a partir da l`onn 2010 l`unitad da datas GG25.</Abstract>
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        <Abstract>La magnetisaziun totala da la crappa sa cumpona da la magnetisaziun inducida che vegn effectuada dal champ magnetic da la terra e da la magnetisaziun remanenta che la crappa ha obtegnì cura ch`ella è vegnida furmada. Divergenzas regiunalas u localas dal champ geomagnetic d`in model global, uschenumnadas anomalias, vegnan mesiradas or da l`aviun. Questas anomalias pon permetter l`identificaziun da las structuras geologicas e tectonicas e da la preschientscha da concentraziuns da minerals. En il rom dal program da retschertgas geofisicalas da la Nagra en il territori da la Svizra dal nord ha la Cumissiun svizra da geofisica mesirà cun aviuns ina rait da 6250 km lingias eromagneticas. Il resultat da questas registraziuns è vegnì preschentà sin 4 chartas a la scala 1:100`000: 2 chartas mussan l`intensitad totala dal champ magnetic (mesirada sin in`autezza da sgol da 1500 m e da 1100 m) e 2 chartas mussan las anomalias residualas suenter avair deducì las tendenzas regiunalas. Las registraziuns na mussan naginas anomalias che permettessan da determinar la profunditad dal sochel e dal foss permocarbonic che sa chatta là. - Charta stampada: E. KLINGELE, 1982. - Charta vectoriala: versiun online, mo las anomalias residualas, E. KLINGELE, 2010.</Abstract>
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        <Abstract>La magnetisaziun totala da la crappa sa cumpona da la magnetisaziun inducida che vegn effectuada dal champ magnetic da la terra e da la magnetisaziun remanenta che la crappa ha obtegnì cura ch`ella è vegnida furmada. Divergenzas regiunalas u localas dal champ geomagnetic d`in model global, uschenumnadas anomalias, vegnan mesiradas or da l`aviun. Questas anomalias pon permetter l`identificaziun da las structuras geologicas e tectonicas e da la preschientscha da concentraziuns da minerals. En il rom dal program da retschertgas geofisicalas da la Nagra en il territori da la Svizra dal nord ha la Cumissiun svizra da geofisica mesirà cun aviuns ina rait da 6250 km lingias eromagneticas. Il resultat da questas registraziuns è vegnì preschentà sin 4 chartas a la scala 1:100`000: 2 chartas mussan l`intensitad totala dal champ magnetic (mesirada sin in`autezza da sgol da 1500 m e da 1100 m) e 2 chartas mussan las anomalias residualas suenter avair deducì las tendenzas regiunalas. Las registraziuns na mussan naginas anomalias che permettessan da determinar la profunditad dal sochel e dal foss permocarbonic che sa chatta là. - Charta stampada: E. KLINGELE, 1982. - Charta vectoriala: versiun online, mo las anomalias residualas, E. KLINGELE, 2010.</Abstract>
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        <Abstract>Las chartas da la periclitaziun tras granella mussan valurs da return da la grondezza dals granels LEHA-100 stimadas statisticamain per la perioda da return da 100 onns. LEHA-100 descriva la pli gronda grondezza da granels spetgada sin ina surfatscha da referenza da 100 m2. Ella vegn deducida da la pli gronda grondezza dal granè spetgada per kilometer quadrat da l`algoritmus dal radar da granella MESHS (datas da radar da MeteoSvizra per ils onns 2002 fin 2020). Las novas chartas da periclitaziun tras granella mussan la grondezza dals granels sco funcziun da la perioda da return T. Ellas descrivan la grondezza dals granels che vegn surpassada sut las cundiziuns climaticas actualas - per la surfatscha da referenza - cun ina probabilitad dad 1/T per onn. Uschia mussa la charta per 100 onns, cun tge grondezza da granels ch`ins sto far quint - a lunga vista - en media ina giada en 100 onns resp. cun ina probabilitad da 2% per onn. Questas chartas èn ina basa actualisada per giuditgar la periclitaziun locala tras granella. La charta da las zonas da granella en l`agiunta G1 da la norma SIA 261/1 (2020) mantegna vinavant sia valaivladad. MESHS: La grondezza dals granels (englais: Maximum Expected Severe Hail Size) è definida sco pli gronda grondezza da granels spetgada per kilometer quadrat. Quai vul dir che la gronda part dals granels sin questa surfatscha è pli pitschna. LEHA: La grondezza dals granels sin la surfatscha da referenza (englais: Largest Expected Hail On A Reference Area) è ina deducziun calculatorica da la grondezza dals granels MESHS che sa referescha al kilometer quadrat. Ella descriva la pli gronda grondezza da granels spetgada sin ina surfatscha da referenza pli pitschna. En il cas extrem po in granè MESHS crudar sin la surfatscha da referenza. Ma quai vegn a capitar mo darar. DOI: https://doi.org/10.18751/Climate/Griddata/CHHC/1.0</Abstract>
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        <Abstract>Las chartas da la periclitaziun tras granella mussan valurs da return da la grondezza dals granels LEHA-100 stimadas statisticamain per la perioda da return da 10 onns. LEHA-100 descriva la pli gronda grondezza da granels spetgada sin ina surfatscha da referenza da 100 m2. Ella vegn deducida da la pli gronda grondezza dal granè spetgada per kilometer quadrat da l`algoritmus dal radar da granella MESHS (datas da radar da MeteoSvizra per ils onns 2002 fin 2020).Las novas chartas da periclitaziun tras granella mussan la grondezza dals granels sco funcziun da la perioda da return T. Ellas descrivan la grondezza dals granels che vegn surpassada sut las cundiziuns climaticas actualas - per la surfatscha da referenza - cun ina probabilitad dad 1/T per onn. Uschia mussa la charta per 50 onns, cun tge grondezza da granels ch`ins sto far quint - a lunga vista - en media ina giada en 50 onns resp. cun ina probabilitad da 2% per onn. Questas chartas èn ina basa actualisada per giuditgar la periclitaziun locala tras granella. La charta da las zonas da granella en l`agiunta G1 da la norma SIA 261/1 (2020) mantegna vinavant sia valaivladad. MESHS: La grondezza dals granels (englais: Maximum Expected Severe Hail Size) è definida sco pli gronda grondezza da granels spetgada per kilometer quadrat. Quai vul dir che la gronda part dals granels sin questa surfatscha è pli pitschna. LEHA: La grondezza dals granels sin la surfatscha da referenza (englais: Largest Expected Hail On A Reference Area) è ina deducziun calculatorica da la grondezza dals granels MESHS che sa referescha al kilometer quadrat. Ella descriva la pli gronda grondezza da granels spetgada sin ina surfatscha da referenza pli pitschna. En il cas extrem po in granè MESHS crudar sin la surfatscha da referenza. Ma quai vegn a capitar mo darar. DOI: https://doi.org/10.18751/Climate/Griddata/CHHC/1.0</Abstract>
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        <Abstract>Las chartas da la periclitaziun tras granella mussan valurs da return da la grondezza dals granels LEHA-100 stimadas statisticamain per la perioda da return da 20 onns. LEHA-100 descriva la pli gronda grondezza da granels spetgada sin ina surfatscha da referenza da 100 m2. Ella vegn deducida da la pli gronda grondezza dal granè spetgada per kilometer quadrat da l`algoritmus dal radar da granella MESHS (datas da radar da MeteoSvizra per ils onns 2002 fin 2020).Las novas chartas da periclitaziun tras granella mussan la grondezza dals granels sco funcziun da la perioda da return T. Ellas descrivan la grondezza dals granels che vegn surpassada sut las cundiziuns climaticas actualas - per la surfatscha da referenza - cun ina probabilitad dad 1/T per onn. Uschia mussa la charta per 20 onns, cun tge grondezza da granels ch`ins sto far quint - a lunga vista - en media ina giada en 20 onns resp. cun ina probabilitad da 2% per onn. Questas chartas èn ina basa actualisada per giuditgar la periclitaziun locala tras granella. La charta da las zonas da granella en l`agiunta G1 da la norma SIA 261/1 (2020) mantegna vinavant sia valaivladad. MESHS: La grondezza dals granels (englais: Maximum Expected Severe Hail Size) è definida sco pli gronda grondezza da granels spetgada per kilometer quadrat. Quai vul dir che la gronda part dals granels sin questa surfatscha è pli pitschna. LEHA: La grondezza dals granels sin la surfatscha da referenza (englais: Largest Expected Hail On A Reference Area) è ina deducziun calculatorica da la grondezza dals granels MESHS che sa referescha al kilometer quadrat. Ella descriva la pli gronda grondezza da granels spetgada sin ina surfatscha da referenza pli pitschna. En il cas extrem po in granè MESHS crudar sin la surfatscha da referenza. Ma quai vegn a capitar mo darar. DOI: https://doi.org/10.18751/Climate/Griddata/CHHC/1.0</Abstract>
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        <Abstract>Las chartas da la periclitaziun tras granella mussan valurs da return da la grondezza dals granels LEHA-100 stimadas statisticamain per la perioda da return da 50 onns. LEHA-100 descriva la pli gronda grondezza da granels spetgada sin ina surfatscha da referenza da 100 m2. Ella vegn deducida da la pli gronda grondezza dal granè spetgada per kilometer quadrat da l`algoritmus dal radar da granella MESHS (datas da radar da MeteoSvizra per ils onns 2002 fin 2020). Las novas chartas da periclitaziun tras granella mussan la grondezza dals granels sco funcziun da la perioda da return T. Ellas descrivan la grondezza dals granels che vegn surpassada sut las cundiziuns climaticas actualas - per la surfatscha da referenza - cun ina probabilitad dad 1/T per onn. Uschia mussa la charta per 50 onns, cun tge grondezza da granels ch`ins sto far quint - a lunga vista - en media ina giada en 50 onns resp. cun ina probabilitad da 2% per onn. Questas chartas èn ina basa actualisada per giuditgar la periclitaziun locala tras granella. La charta da las zonas da granella en l`agiunta G1 da la norma SIA 261/1 (2020) mantegna vinavant sia valaivladad. LEHA: La grondezza dals granels sin la surfatscha da referenza (englais: Largest Expected Hail On A Reference Area) è ina deducziun calculatorica da la grondezza dals granels MESHS che sa referescha al kilometer quadrat. Ella descriva la pli gronda grondezza da granels spetgada sin ina surfatscha da referenza pli pitschna. En il cas extrem po in granè MESHS crudar sin la surfatscha da referenza. Ma quai vegn a capitar mo darar. DOI: https://doi.org/10.18751/Climate/Griddata/CHHC/1.0</Abstract>
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        <Abstract>Qua sa tracti da l`aua che vegn retegnida en il terren da las forzas da tensiun e che po vegnir absorbada bain da las plantas (tensiun da tschitsch 0,1 - 1 atm). Per 1 cm profunditad fisiologica poi vegnir fatg quint approximativamain cun 1 mm d`aua bain absorbabla (0,1 - 1 atm tensiun da tschitsch). La profunditad fisiologica resulta da tut la stresa penetrabla da ragischs minus la pedrusitad e gronds chaviertgs en terrens da sablun e da gera, sco er minus structuras cumpactas ed orizonts cun pauc oxigen. (Detagls: charta da l`adattaziun dal terren da la Svizra, mars 1980)</Abstract>
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        <Abstract>Charta davart la ristga d`erosiun dal terren cultivà, perdita media da terren en tonnas/(ha*onn) (Uffizi federal d`agricultura)Charta davart la ristga d`erosiun dal terren cultivà en Svizra en in raster da 2x2 meters sin basa da swissALTI3D e da datas chantunalas davart la surfatscha d`er (stadi 2021). La charta mussa la media da blers onns da la perdita potenziala da terren en tonnas per hectara ed onn, calculada sin basa da terren nuncultivà blut (erosiun che pudess capitar teoreticamain, sch`il terren fiss adina blut). Nianzas da colur verdas correspundan ad ina ristga d`erosiun pitschna, nianzas melnas ad ina ristga d`erosiun mesauna e nianzas cotschnas ad ina ristga d`erosiun auta. Las valurs calculadas en il model èn tuttas pli autas ch`en realitad (ca. 10 giadas), perquai che l`elavuraziun e la cultivaziun dal terren èn vegnidas exclusas (factur C) ed integradas en la calculaziun sco constanta cun la valur 1. La calculaziun da la ristga d`erosiun cun algoritmus da `multiple flow` permetta da preschentar la structura dal terren en moda precisa e detagliada - p.ex. la structura da foppas u da spundas traversalas taissas - e d`identifitgar uschia p.ex. er la ristga d`erosiun da la lingia la pli bassa. Quai è illustrà detagliadamain en la charta da deflussiun da l`aua (guardar la charta da deflussiun da l`aua). La basa spaziala per la calculaziun furman blocs da parcellas (guardar la charta da blocs da parcellas).</Abstract>
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        <Abstract>Blocs da parcellas èn surfatschas colliadas che pon vegnir duvradas per l`agricultura che han cunfins exteriurs relativamain stabils e percorschibels en la natira (p.ex. guauds, vias, surfatschas surbajegiadas, auas, foss). Sco basa da calculaziun serva il model topografic da la cuntrada MTC3D. In bloc da parcellas è pia in intschess idrologic serrà, nua che tut ils pixels pon esser colliads in cun l`auter idrologicamain e pon uschia s`influenzar concernent l`erosiun. En il model na pon auters blocs da parcellas u autras surfatschas ordaifer in bloc da parcellas betg influenzar il fluss d`aua e l`erosiun entaifer in bloc da parcellas. En il model n`è l`afflussiun d`aua estra pia betg pussaivla. La grondezza minimala d`in bloc da parcellas è vegnida fixada a 25 aras. La surveglianza da l`erosiun sin surfatschas d`ers tras las autoritads cumpetentas vegn fatga il meglier cun controllar ils blocs da parcellas en las regiuns prioritaras. La ristga d`erosiun sto vegnir calculada da nov, sche la grondezza dals blocs da parcellas sa mida p.ex. pervia da la construcziun da vias novas u sche chaglioms vegnan plantads u allontanads.</Abstract>
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        <Abstract>La charta potenziala da las surfatschas colliadas cun auas da surfatscha mussa en ina spezia d`in &#39;scenari dal mender cas pussaivel&#39; (terren nuncultivà permanentamain blut, naginas strivlas da plimatsch u mesiras architectonicas) surfatschas, tar las qualas i sto vegnir fatg quint cun in privel considerabel d`immissiuns da substanzas en las auas, sche questas surfatschas na vegnan betg cultivadas en ina moda confurma al lieu. Ella è pia in med d`agid per planisar sistematicamain las mesiras per proteger las auas. Il model per identifitgar la colliaziun cun auas da surfatscha da las surfatschas agriculas ch`èn potenzialmain periclitadas da l`erosiun sa basa sin la CRE2. Cun il model da las surfatschas colliadas cun auas da surfatscha po vegnir calculada la probabilitad d`ina colliaziun cun in`aua per mintga cella da raster da la CRE2. Per arrivar dal model da colliaziun potenzial al model actual da colliaziun cun in`aua vegnan duvradas infurmaziuns davart l`utilisaziun da las surfatschas periclitadas e d`eventualas mesiras che reduceschan la deflussiun. Quellas ston vegnir procuradas al lieu.</Abstract>
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        <Abstract>Sco cumplettaziun da la charta da las surfatschas colliadas cun auas da surfatscha è er vegnida fatga ina charta che differenziescha tranter ina colliaziun directa ed ina colliaziun indirecta cun in`aua. Surfatschas che han ina colliaziun directa cun in`aua sa chattan sper in`aua u en colliadas cun l`aua sur foss che mainan temporarmain aua u sur lingias da profunditad. Sur tumbins da drenascha u sur tumbins d`entrada da l`allontanament da l`aua da la via po l`aua da surfatscha er arrivar indirectamain en las auas. Grazia a questas infurmaziuns pon las mesiras cunter l`immissiun da substanzas en l`aua eventualmain vegnir planisadas en moda anc pli precisa. I vegnan differenziadas 6 categorias da la probabilitad che las surfatschas agriculas èn colliadas cun auas.</Abstract>
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        <Abstract>Sin ils quatter fegls da la charta da la scala 1:200`000 è represchentà in giudicament general da las premissas climaticas e da las restricziuns per l`agricultura, dividì en 20 categorias. La charta vul mussar las differenzas considerablas da las pussaivladads da cultivar products agriculs en las singulas regiuns.</Abstract>
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        <Abstract>Cun il register da las denominaziuns d`origin protegidas (DOP/AOC) e da las indicaziuns geograficas protegidas (IGP) pon vegnir protegids ils nums dal territori e las denominaziuns tradiziunalas da products agriculs (cun excepziun dal vin), dals quals la qualitad e las caracteristicas principalas vegnan determinadas da lur derivanza geografica. Sch`in num è protegì, dastga el vegnir duvrà mo dals producents da quel territori geografic determinà che observan in carnet d`obligaziuns detaglià. L`intent da proteger tschertas denominaziuns da products agriculs è quel da preservar ils consuments d`in engion e d`impedir - en l`interess dals purs - la concurrenza illoiala tar l`applicaziun da questas noziuns. Las regulaziuns en quest sectur pussibiliteschan la renconuschientscha vicendaivla da products da qualitad tranter la Svizra e l`Uniun europeica. Differenziadas vegnan las 4 categorias chaschiel, products da charn, products da plantas e spirituosas. Actualmain èn inscrits vers 30 differents products en il register da las denominaziuns d`origin protegidas e cuntinuadamain vegnan vitiers novs.</Abstract>
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        <Abstract>Dapi l`onn 1995 vegnan definidas coordinatas per tut ils lieus da lavur che vegnan registrads en las dumbraziuns federalas dals manaschis. Numerusas caracteristicas davart ils manaschis e davart las persunas occupadas da tut ils secturs economics, tenor plazzas a temp cumplain e parzial e tenor la NOGA (sistematica generala da las branschas economicas) vegnan agregadas suenter mintga retschertga per hectara e stattan a disposiziun sco geodatas. A partir da l`onn 2011 è la dumbraziun dals manaschis vegnida remplazzada tras la Statistica da la structura d`interpresas (STATENT), ina retschertga cumpletta sin basa dals registers da las cassas da cumpensaziun da la AVS che vegn actualisada mintga onn. La STATENT furnescha infurmaziuns centralas davart la structura da l`economia svizra (p.ex. dumber da manaschis, dumber da lieus da lavur, dumber da persunas occupadas e.u.v) e dat uschia ina survista da la cuntrada economica da la Svizra. In lieu da lavur correspunda ad in manaschi u ad ina part d`in manaschi (lavuratori, fabrica e.u.v.) che sa chatta en in lieu definibel topograficamain. Là exequeschan ina u pliras persunas activitads per il medem manaschi.</Abstract>
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        <Abstract>Dapi l`onn 1995 vegnan definidas coordinatas per tut ils lieus da lavur che vegnan registrads en las dumbraziuns federalas dals manaschis. Numerusas caracteristicas davart ils manaschis e davart las persunas occupadas da tut ils secturs economics, tenor plazzas a temp cumplain e parzial e tenor la NOGA (sistematica generala da las branschas economicas) vegnan agregadas suenter mintga retschertga per hectara e stattan a disposiziun sco geodatas. A partir da l`onn 2011 è la dumbraziun dals manaschis vegnida remplazzada tras la statistica da la structura d`interpresas (STATENT), ina retschertga cumpletta sin basa dals registers da las cassas da cumpensaziun da la AVS che vegn actualisada mintga onn. La STATENT furnescha infurmaziuns centralas davart la structura da l`economia svizra (p.ex. dumber da manaschis, dumber da lieus da lavur, dumber da persunas occupadas e.u.v) e dat pia ina survista da la cuntrada economica da la Svizra. Per l`occupaziun en equivalents a temp cumplain (ETC) vegn transfurmà il volumen da lavur da tut las persunas che lavuran a temp cumplain ed a temp parzial, che vegn normalmain calculà en uras da lavur, en persunas che lavuran a temp cumplain.</Abstract>
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        <Abstract>La mesiraziun da la distanza tar servetschs per mintga hectara abitada en Svizra metta a disposiziun infurmaziuns statisticas multifaras davart l`access a bains, a servetschs sco er a lieus da recreaziun. In provediment da basa suffizient cun ils bains e cun ils servetschs che vegnan duvrads en il mintgadi sco er l`access a lieus da recreaziun sco rivas da lais u guauds èn da gronda impurtanza per la qualitad da viver. La calculaziun da la cuntanschibladad da quests servetschs è ina metoda per mesirar quest fenomen. La cuntanschibladad vegn operaziunalisada tras la distanza che vegn percurrida sin la rait da vias tranter il lieu da domicil ed il lieu dal proxim furnitur da servetschs resp. dal proxim lieu da recreaziun.</Abstract>
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        <Abstract>La mesiraziun da la distanza tar servetschs per mintga hectara abitada en Svizra metta a disposiziun infurmaziuns statisticas multifaras davart l`access a bains, a servetschs sco er a lieus da recreaziun.  In provediment da basa suffizient cun ils bains e cun ils servetschs che vegnan duvrads en il mintgadi sco er l`access a lieus da recreaziun sco rivas da lais u guauds èn da gronda impurtanza per la qualitad da viver. La calculaziun da la cuntanschibladad da quests servetschs è ina metoda per mesirar quest fenomen. La cuntanschibladad vegn operaziunalisada tras la distanza che vegn percurrida sin la rait da vias tranter il lieu da domicil ed il lieu dal proxim furnitur da servetschs resp. dal proxim lieu da recreaziun.</Abstract>
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        <Abstract>Il register federal dals edifizis e da las abitaziuns (REA) è vegnì stabilì a maun da datas da la dumbraziun dal pievel 2000 per intents statistics.Il REA n`è betg sco ultim s`etablì grazia a la revisiun totala da l`ordinaziun (OREA), ch`è entrada en vigur il 1. da fanadur 2017, sco sistem d`infurmaziun naziunal decisiv per ils edifizis. Il REA cuntegna infurmaziuns davart projects da construcziun, edifizis, abitaziuns, entradas d`edifizis e vias. Las datas dal stgalim A èn publicas e pon vegnir utilisadas senza restricziuns. Il nivel da datas `REA: funtauna d`energia/da chalur dal stgaudament` illustrescha graficamain (colur) la funtauna d`energia/da chalur dal sistem da stgaudar cun la pli auta prestaziun e la data d`actualisaziun relativa (furma).</Abstract>
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        <Abstract>Per las chartas e per las preschentaziuns tematicas en pitschnas scalas èn savens giavischads cunfins administrativs che demussan in bass grad da precisaziun. Ils cunfins communals digitals da la Svizra e dal Principadi da Liechtenstein, che vegnan actualisads annualmain tras l`Uffizi federal da topografia, èn savens memia detagliads. Perquai metta GEOSTAT a disposiziun cunfins digitals da las vischnancas, dals districts, dals chantuns, da las regiuns grondas, dals lais cun passa 5 km2 surfatscha sco er cunfins naziunals en differentas generalisaziuns. Supplementarmain a las unitads administrativas èn er ils cunfins dal territori cun caracter urban (aglomeraziuns incl. vischnancas respectivas a l`exteriur e centers ordaifer las aglomeraziuns) disponibels sin in agen nivel da datas. Il nivel da generalisaziun G1 è adattà particularmain per preschentaziuns cartograficas da las scalas 1:250`000 fin 1:500`000.</Abstract>
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        <Abstract>Ina lingia da construcziun garantescha il basegn da spazi per la gestiun, per la renovaziun u per l`engrondiment d`in implant da current ferm. Tranter ina lingia da construcziun ed in implant da current ferm na dastga vegnir construì nagut che impedescha la gestiun, la renovaziun u l`engrondiment da quest implant da current ferm. La gestiunaria d`ina rait po dumandar lingias da construcziun.Ina lingia da construcziun po restrenscher las proprietarias ed ils proprietaris dals bains immobigliars pertutgads. Per quest motiv èn las lingias da construcziun inscrittas en il cataster da las restricziuns da dretg public da la proprietad (cataster RDPP). Questa unitad da datas cuntegna tut las lingias da construcziun valaivlas. Ella cuntegna er tut las lingias da construcziun dumandadas, sch`il chantun ch`è cumpetent per l`exposiziun publica utilisescha il cataster RDPP.</Abstract>
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        <Abstract>In indriz per producir electricitad è in indriz tecnic, cun il qual vegn producida electricitad. Igl è d`interess general d`avair ina survista spaziala da tut ils indrizs per producir electricitad da la Svizra. En spezial duai l`augment dals indrizs che produceschan electricitad sin basa da funtaunas regenerablas vegnir mussà en moda transparenta. Ultra da quai po vegnir rendida visibla la relaziun dals indrizs che produceschan electricitad sin basa da funtaunas regenerablas envers ils indrizs che produceschan electricitad sin basa da funtaunas betg regenerablas. I vegn differenzià tranter forza idraulica, fotovoltaica, energia da vent, biomassa, geotermia, energia nucleara, ieli mineral, gas natiral e charvun. Quest effectiv da datas cuntegna tut ils indrizs per producir electricitad ch`èn registrads en il Sistem svizzer da garanzia d`origin. Latiers tutgan per l`ina tut ils indrizs cun ina prestaziun da pli che 30 kilovoltampere (kVA), sco er indrizs pitschens (pli gronds che 2 kilowatt) ch`èn vegnids registrads voluntarmain per survegnir la garanzia d`origin (GO). Per l`autra cuntegna l`effectiv da datas indrizs che vegnan promovids d`ina indemnisaziun per cuvrir ils custs da la furniziun d`electricitad, d`ina indemnisaziun unica, d`ina finanziaziun dals custs supplementars u d`ina contribuziun d`investiziun (tenor ils art. 19 e 24 LEn). I èn cuntegnids mo indrizs per producir electricitad ch`èn en funcziun.</Abstract>
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      <Abstract>Minergie-Areal Das Minergie-Areal verbindet Neu- und Bestandsbauten zu einem effizienten, komfortablen und zukunftssicheren Lebensraum. Durch minimalen Energieverbrauch, maximale Nutzung erneuerbarer Energien und stark reduzierte Treibhausgasemissionen setzt es hohe Massstäbe im Klimaschutz. Die Neubauten erfüllen die Minergie-Standards, während die Bestandsbauten energetisch saniert werden. Das professionelle Areal-Management sichert einen optimalen Betrieb sowie ein effizientes Monitoring. Gemeinsame Infrastrukturen, Abwärmenutzung und Photovoltaik optimieren die Energieversorgung. Begrünung, schattenspendende Bäume und das Schwammstadt-Prinzip schaffen klimaangepasste Aussenräume. Ein cleveres Fuss- und Velonetz, ausreichend Abstellplätze sowie Sharing-Angebote für E-Autos oder Lastenräder fördern klimafreundliche Mobilität. Link: https://www.minergie.ch/de/standards/neubau/minergie-areal/ SNBS-Areal Wie das SNBS-Areal erlaubt der SNBS-Hochbau eine umfassende Betrachtung in den Bereichen Gesellschaft, Wirtschaft und Umwelt. Der Standard bietet Entwickelnden Architektinnen und Architekten sowie Fachplanenden bei der Erfüllung der Anforderungen, und damit bei der Gestaltung des Areals, grossen Freiraum - sowohl bei Neubauten als auch bei Erneuerungen. Einzelne Bauten werden nur insoweit betrachtet, als sie einen Einfluss auf das Areal haben. Der `Blick ins Gebäude` ist somit weniger tief - wichtiger ist vielmehr die nachhaltige Verbesserung der Arealeigenschaften. Mit dem Benotungssystem, bei dem das arithmetische Mittel aller Einzelnoten die Gesamtnote ergibt, können individuelle Schwerpunkte in einzelnen Bereichen gesetzt und notenmässig bis zu einem gewissen Grad kompensiert werden. Link: https://www.snbs-hochbau.ch/standards/snbs-areal/ 2000-Watt-Areale Das Label `2000-Watt-Areale` wurde durch die beiden oben genannten Labels SNBS und Minergie ersetzt. Die historischen Daten sind in die vollständige Ebene integriert. Das Label für 2000-Watt-Areale zeichnet Siedlungsgebiete aus, die einen nachhaltigen Umgang mit Ressourcen für die Erstellung von Gebäuden, deren Betrieb und Erneuerung und die durch den Betrieb verursachte Mobilität gesamthaft nachweisen können. Das Zertifikat ist auf Grundlage des bekannten Energiestadt-Labels in Kombination mit dem SIA-Effizienzpfad Energie für Gebäude aufgebaut. Für die Arealentwicklung kann das Zertifikat schon in einer frühen Projektphase beantragt werden und wird nach der Bewertung der Projektziele und der verpflichtenden Vereinbarung zur Einhaltung dieser Ziele erteilt. Das Zertifikat für eine Arealentwicklung kann solange erteilt werden, bis mehr als 50% der Gebäudeflächen der bestimmungsgemässen neuen Nutzung übergeben sind. Folgend muss sich das Areal einer neu aufgelegten Zertifizierung im Betrieb beweisen. Das Label beruht auf der Beurteilung vom Management-System, von Kommunikation und Kooperation, der Gebäudeerstellung und des Betriebs, der Ver- und Entsorgung sowie der Mobilität.</Abstract>
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        <Abstract>Tras la cussegliaziun d`impuls `stgaudar en moda regenerabla` vegnan las proprietarias ed ils proprietaris d`edifizis cun in stgaudament d`ieli, da gas u electric vegnan a savair, cun tge funtaunas da chalur regenerablas che lur edifizi po vegnir stgaudà en moda raschunaivla e cun paucas emissiuns da CO2. Tar la consultaziun d`impuls `stgaudar en moda regenerabla` vegn ina cussegliadra u in cussegliader a chasa tar la clienta u il client (proprietaria u proprietari da l`edifizi). En il discurs da cussegliaziun vegni eruì il basegn d`energia da l`edifizi, ils facturs specifics per il lieu ed ils giavischs da la proprietaria u dal proprietari. La cussegliadra u il cussegliader examinescha quests facturs e surdat a la proprietaria u al proprietari da l`edifizi ina glista da controlla cun la situaziun actuala e cun las recumandaziuns concernent la midada dal sistem da stgaudar. La glista da controlla è ina buna basa per dumandar las dretgas offertas e per iniziar in project da construcziun cun success. Quest effectiv da datas cuntegna tut las cussegliadras e tut ils cussegliaders d`impuls ch`èn vegnids scolads en il rom dal program `stgaudar en moda regenerabla` e che adempleschan ils criteris da qualitad.</Abstract>
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        <Abstract>Proprietarias e proprietaris d`edifizis e d`abitaziuns cun in stgaudament d`ieli, da gas u electric vegnan a savair tras la cussegliaziun d`impuls per stgaudar cun energia regenerabla, cun tge funtaunas da chalur regenerablas che lur edifizi po vegnir stgaudà en moda raschunaivla e cun ina pitschna producziun da CO2. Tar la cussegliaziun d`impuls per stgaudar cun energia regenerabla vegn ina cussegliadra u in cussegliader a chasa tar la clienta u il client (proprietarias e proprietaris da l`edifizi/administratur[a]s/cuminanzas da proprietaris en condomini). En il discurs da cussegliaziun vegnan eruids il basegn d`energia da l`edifizi, ils facturs specifics per il lieu ed ils giavischs da la proprietaria u dal proprietari. La cussegliadra u il cussegliader examinescha quests facturs e surdat a la proprietaria u al proprietari da l`edifizi u a la cuminanza da proprietaris en condomini ina glista da controlla cun la situaziun actuala e cun las recumandaziuns concernent la midada dal sistem da stgaudar. La glista da controlla è ina buna basa per eventualmain dar l`incumbensa per ina cumparegliaziun da variantas, per sa laschar far las gistas offertas e per lantschar cun success in project da construcziun. Quest effectiv da datas cuntegna tut las cussegliadras ed ils cussegliaders d`impuls scolads en il rom dal program per stgaudar cun energia regenerabla, che adempleschan ils criteris da qualitad.</Abstract>
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        <Abstract>La dumonda da chalur e da fradur è d`ina impurtanza centrala per la planisaziun strategica da raits termicas. La construcziun d`ina rait termica en in territori renda pir, cur che la dumonda da chalur e/u da fradur è gronda avunda. En la planisaziun strategica serva la dumonda da chalur ad identifitgar territoris pli gronds ch`èn colliads in cun l`auter e che pudessan s`adattar per ina rait termica. A partir d`ina densitad da chalur da 700 MWh/a per hectara vala in territori sco adattà. Ultra da la densitad da chalur è er il nivel da temperatura necessari impurtant per il provediment da chalur. L`industria ed il mastergn dovran per part chalur da process d`in nivel fitg aut (per part 1000 °C e dapli). Quella na po betg vegnir messa a disposiziun cun ina rait termica. Pervia da quai è la dumonda da chalur da l`industria vegnida registrada en in`atgna unitad da datas. La dumonda da chalur d`edifizis d`abitar e da servetschs è la pli interessanta per raits termicas, perquai che la maioritad dals edifizis da questa categoria po vegnir provedida cun temperaturas bassas da ca. 12°C fin maximal 90°C. La basa da datas furma la Statistica dals edifizis e da las abitaziuns (SEA) da l`onn 2014 e la Statistica da la structura d`interpresas (STATENT) dal UST da l`onn 2013, cumplettada cun cifras dal rapport annual `Consum d`energia en l`industria ed en il sectur da servetschs` da l`Uffizi federal d`energia (UFE). La dumonda da chalur vegn visualisada sco densitad da chalur en il raster da hectaras. La densitad da chalur vegn mussada a maun d`ina scala da colurs. Las indicaziuns servan sco material d`infurmaziun per la publicitad e n`èn betg infurmaziuns uffizialas u explicaziuns giuridicamain liantas.</Abstract>
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        <Abstract>En Svizra sa chattan ils territoris potenzials per energia da vent tranter auter sin las collinas dal Giura, sco er en las Alps ed en las Prealps. Durant ils mais d`enviern ha l`aria là regularmain e per in temp pli lung ina temperatura da main che 0° celsius. Colliads cun quai èn effects d`englatschament vi d`instruments da mesiraziun e vi da las palas dals roturs. L`englatschament influenzescha la planisaziun ed il manaschi d`in implant d`energia da vent (IEV) a differenta moda: glatsch sin las palas dal rotur disturba l`erodinamica da las palas e chaschuna perditas da producziun. Il pais supplementar ed il dischequiliber da las palas ch`èn colliads cun l`englatschament engrevgeschan ils elements structurals dals IEV. Per motivs da segirezza (glatsch che vegn schlavazzà davent) e sin basa da la chargia supplementara per il material vegnan ils IEV serrads giu en cas d`in englatschament. Plinavant po l`englatschament dals instruments d`in IEV che mesiran il vent disturbar ses funcziunament. Las calculaziuns quant savens ch`i dat englatschaments sa basa sin datas naziunalas davart l`aua dals nivels, davart la temperatura e davart il vent che derivan da l`analisa dal model da la previsiun da l`aura COSMO-2 da MeteoSvizra. Il model d`englatschament calculescha la chargia da glatsch vi d`ina structura cilindrica che rotescha libramain. La frequenza d`englatschaments vegn mussada sin in raster da 2,2 km ed è vegnida verifitgada a maun da mesiraziuns da staziuns IMIS en las Alps e da mesiraziuns sin il Giura. La charta mussa quant savens ch`i ha dà englatschaments meteorologics sin 100 m sur il terren per la perioda da l`avust 2007 fin il fanadur 2009. En la media da 10 onns è la media dals englatschaments var 5 % pli bassa. Las indicaziuns da la frequenza èn valurs modelladas. Ellas infurmeschan, nua ch`i po dar englatschaments en Svizra. Las indicaziuns da la frequenza na pon betg vegnir interpretadas sco valurs exactas per in tschert punct. Sche la topografia è structurada fermamain, sco che quai è savens il cas en las Alps centralas, datti divergenzas. En lieus exponids fermamain datti pli savens englatschaments, en lieus protegids datti main englatschaments che mussà sin la charta. Sin la charta vegnan mussadas las cundiziuns meteorologicas, durant las qualas i po dar englatschaments, las periodas d`englatschament dals instruments duran en media pli ditg. Sch`in interess per il svilup d`in tschert lieu è avant maun, ston vegnir fatgas mesiraziuns al lieu.</Abstract>
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        <Abstract>Minergie è dapi l`onn 1998 il standard architectonic svizzer per confort, effizienza e mantegniment da la valur. La marca vegn purtada cuminaivlamain da l`economia, dals chantuns e da la Confederaziun ed è protegida cunter abus. En il center stat il confort d`abitar e da lavurar da las persunas che utiliseschan in edifizi, e quai tant tar construcziuns novas sco er tar renovaziuns. Ina rolla speziala giogan en quest connex l`auta qualitad dals mirs exteriurs d`in edifizi ed ina ventilaziun controllada. Caracteristic per edifizis da Minergie èn ultra da quai in basegn d`energia fitg bass ed ina quota uschè gronda sco pussaivel d`energias regenerablas. La qualitad da construcziun vegn quantifitgada tras il consum d`energia specific per meter quadrat da surfatscha che retira energia (SRE). Ils trais standards architectonics enconuschents Minergie, Minergie-P e Minergie-A garanteschan gia en la fasa da planisaziun in`excellenta qualitad ed effizienza. Il standard Minergie per edifizis cun in pitschen consum d`energia sa drizza a patrun da construcziun ed a planisaders cun pretensiuns surproporziunalas a la qualitad, al confort ed a l`energia. Minergie-P designescha edifizis cun in consum d`energia fitg pitschen ed ademplescha pretensiuns maximalas a la qualitad, al confort ed a l`energia. En spezial pervia da mirs exteriurs d`in edifizi d`ina excellenta qualitad. Minergie-A cumbinescha pretensiuns grondissimas a la qualitad ed al confort cun ina independenza energetica maximala, e quai grazia ad in implant grond da fotovoltaica, ad ina battaria ed ad in management da la chargia. Cumplettads vegn quels da trais products supplementars cumbinabels libramain: ECO resguarda ils temas da la sanadad e da l`ecologia architectonica. SQM construcziun sa drizza a patruns da construcziun ed a planisaders che vulessan avair garantì las directivas pretensiusas a la construcziun. SQM gestiun optimescha l`utilisaziun dals indrizs da la tecnica da chasa e garantescha uschia in confort maximal. Actualmain han en Svizra passa 39 600 edifizis il certificat Minergie, passa 3600 edifizis il certificat Minergie-P e passa 550 edifizis il certificat Minergie-A.</Abstract>
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        <Abstract>La chalur da lais e da flums è ina funtauna d`energia termica gronda, ma pauc utilisada. En Svizra pudess questa funtauna d`energia regenerabla vegnir utilisada per stgaudar (retratga da chalur) e per sfradentar (inducziun da chalur), perquai che bleras citads sa chattan sper lais e flums e perquai che la tecnica è etablida bain.Sa basond sin simplas ipotesas è vegnì stimà il potenzial dals lais e dals flums ils pli gronds da la Svizra areguard la retratga e l`inducziun da chalur. En quest connex èn qualitads specificas da las auas vegnidas resguardadas mo per part. Ils potenzials ston vegnir chapids sco valurs directivas e na duessan perquai betg vegnir duvrads sco basa da planisaziun definitiva. La stimaziun è vegnida fatga da la Eawag (Institut federal per provediment, serenaziun e protecziun da las auas da la SPF) e finanziada da l`Uffizi federal d`ambient. Questa unitad da datas cuntegna il potenzial dals lais e dals flums ils pli gronds da la Svizra areguard la retratga e l`inducziun da chalur.</Abstract>
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        <Abstract>L`atlas dal vent da la Svizra descriva las relaziuns da vent per 5 autezzas sur il terren: 50, 75, 100, 125 e 150 m. Las datas sa basan sin ina modellaziun per tut la Svizra cun ina ladezza orizontala dal raster da 100 m. En la charta vegn mussada la media annuala da la sveltezza dal vent modellada per mintga punct dal raster. La repartiziun da las sveltezzas dal vent en classas da sveltezza dal vent po vegnir mussada approximativamain cun ils parameters Weibull A (parameter da scala) e k (parameter da furma). La media da la sveltezza dal vent na po betg vegnir deducida directamain dals parameters da Weibull, perquai ch`i sa tracta d`ina approximaziun a la repartiziun dal vent e perquai che quella na po betg vegnir reproducida suffizientamain per mintga lieu. La rosa dals vents mussa la frequenza relativa da las direcziuns dal vent modelladas. Las sveltezzas dal vent medias ed ils parameters da Weibull respectivs vegnan inditgads per sectur. Per calcular las sveltezzas e las direcziuns dal vent èn vegnidas resguardadas en la modellaziun las datas da mesiraziuns da blers onns. Perquai che las staziuns da mesiraziun n`èn betg avant maun en la medema spessezza en tut las regiuns da la Svizra e perquai ch`i dat inexactadads tar la modellaziun da las circulaziuns dals vents en in las cuntradas cun ina topografia cumplexa, n`èn ils resultats betg dal tuttafatg libers da malsegirezzas. La dimensiun da las malsegirezzas sa chatta en l`artg dal Giura tar fin a +/- 0,5 m/s, en la Svizra centrala tar fin a +/- 0,7 m/s, en las Prealps tar fin a +/- 0,5 m/s ed en las Alps tar fin a +/- 1,3 m/s. Per las chartas davent d`ina autezza da 100m sur il terren stattan a disposiziun marcantamain main mesiraziuns per la modellaziun. Uschia resulta ina intschertezza pli gronda dals resultats. Las indicaziuns ston vegnir chapidas sco valitaziun approximativa da las relaziuns da vent. Sch`in interess per il svilup d`in tschert lieu è avant maun, ston vegnir fatgas mesiraziuns al lieu.</Abstract>
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        <Abstract>L`atlas dal vent da la Svizra descriva las relaziuns da vent per 5 autezzas sur il terren: 50, 75, 100, 125 e 150 m. Las datas sa basan sin ina modellaziun per tut la Svizra cun ina ladezza orizontala dal raster da 100 m. En la charta vegn mussada la media annuala da la sveltezza dal vent modellada per mintga punct dal raster. La repartiziun da las sveltezzas dal vent en classas da sveltezza dal vent po vegnir mussada approximativamain cun ils parameters Weibull A (parameter da scala) e k (parameter da furma). La media da la sveltezza dal vent na po betg vegnir deducida directamain dals parameters da Weibull, perquai ch`i sa tracta d`ina approximaziun a la repartiziun dal vent e perquai che quella na po betg vegnir reproducida suffizientamain per mintga lieu. La rosa dals vents mussa la frequenza relativa da las direcziuns dal vent modelladas. Las sveltezzas dal vent medias ed ils parameters da Weibull respectivs vegnan inditgads per sectur. Per calcular las sveltezzas e las direcziuns dal vent èn vegnidas resguardadas en la modellaziun las datas da mesiraziuns da blers onns. Perquai che las staziuns da mesiraziun n`èn betg avant maun en la medema spessezza en tut las regiuns da la Svizra e perquai ch`i dat inexactadads tar la modellaziun da las circulaziuns dals vents en in las cuntradas cun ina topografia cumplexa, n`èn ils resultats betg dal tuttafatg libers da malsegirezzas. La dimensiun da las malsegirezzas sa chatta en l`artg dal Giura tar fin a +/- 0,5 m/s, en la Svizra centrala tar fin a +/- 0,7 m/s, en las Prealps tar fin a +/- 0,5 m/s ed en las Alps tar fin a +/- 1,3 m/s. Per las chartas davent d`ina autezza da 100m sur il terren stattan a disposiziun marcantamain main mesiraziuns per la modellaziun. Uschia resulta ina intschertezza pli gronda dals resultats. Las indicaziuns ston vegnir chapidas sco valitaziun approximativa da las relaziuns da vent. Sch`in interess per il svilup d`in tschert lieu è avant maun, ston vegnir fatgas mesiraziuns al lieu.</Abstract>
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        <Abstract>L`atlas dal vent da la Svizra descriva las relaziuns da vent per 5 autezzas sur il terren: 50, 75, 100, 125 e 150 m. Las datas sa basan sin ina modellaziun per tut la Svizra cun ina ladezza orizontala dal raster da 100 m. En la charta vegn mussada la media annuala da la sveltezza dal vent modellada per mintga punct dal raster. La repartiziun da las sveltezzas dal vent en classas da sveltezza dal vent po vegnir mussada approximativamain cun ils parameters Weibull A (parameter da scala) e k (parameter da furma). La media da la sveltezza dal vent na po betg vegnir deducida directamain dals parameters da Weibull, perquai ch`i sa tracta d`ina approximaziun a la repartiziun dal vent e perquai che quella na po betg vegnir reproducida suffizientamain per mintga lieu. La rosa dals vents mussa la frequenza relativa da las direcziuns dal vent modelladas. Las sveltezzas dal vent medias ed ils parameters da Weibull respectivs vegnan inditgads per sectur. Per calcular las sveltezzas e las direcziuns dal vent èn vegnidas resguardadas en la modellaziun las datas da mesiraziuns da blers onns. Perquai che las staziuns da mesiraziun n`èn betg avant maun en la medema spessezza en tut las regiuns da la Svizra e perquai ch`i dat inexactadads tar la modellaziun da las circulaziuns dals vents en in las cuntradas cun ina topografia cumplexa, n`èn ils resultats betg dal tuttafatg libers da malsegirezzas. La dimensiun da las malsegirezzas sa chatta en l`artg dal Giura tar fin a +/- 0,5 m/s, en la Svizra centrala tar fin a +/- 0,7 m/s, en las Prealps tar fin a +/- 0,5 m/s ed en las Alps tar fin a +/- 1,3 m/s. Per las chartas davent d`ina autezza da 100m sur il terren stattan a disposiziun marcantamain main mesiraziuns per la modellaziun. Uschia resulta ina intschertezza pli gronda dals resultats. Las indicaziuns ston vegnir chapidas sco valitaziun approximativa da las relaziuns da vent. Sch`in interess per il svilup d`in tschert lieu è avant maun, ston vegnir fatgas mesiraziuns al lieu.</Abstract>
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        <Abstract>L`atlas dal vent da la Svizra descriva las relaziuns da vent per 5 autezzas sur il terren: 50, 75, 100, 125 e 150 m. Las datas sa basan sin ina modellaziun per tut la Svizra cun ina ladezza orizontala dal raster da 100 m. En la charta vegn mussada la media annuala da la sveltezza dal vent modellada per mintga punct dal raster. La repartiziun da las sveltezzas dal vent en classas da sveltezza dal vent po vegnir mussada approximativamain cun ils parameters Weibull A (parameter da scala) e k (parameter da furma). La media da la sveltezza dal vent na po betg vegnir deducida directamain dals parameters da Weibull, perquai ch`i sa tracta d`ina approximaziun a la repartiziun dal vent e perquai che quella na po betg vegnir reproducida suffizientamain per mintga lieu. La rosa dals vents mussa la frequenza relativa da las direcziuns dal vent modelladas. Las sveltezzas dal vent medias ed ils parameters da Weibull respectivs vegnan inditgads per sectur. Per calcular las sveltezzas e las direcziuns dal vent èn vegnidas resguardadas en la modellaziun las datas da mesiraziuns da blers onns. Perquai che las staziuns da mesiraziun n`èn betg avant maun en la medema spessezza en tut las regiuns da la Svizra e perquai ch`i dat inexactadads tar la modellaziun da las circulaziuns dals vents en in las cuntradas cun ina topografia cumplexa, n`èn ils resultats betg dal tuttafatg libers da malsegirezzas. La dimensiun da las malsegirezzas sa chatta en l`artg dal Giura tar fin a +/- 0,5 m/s, en la Svizra centrala tar fin a +/- 0,7 m/s, en las Prealps tar fin a +/- 0,5 m/s ed en las Alps tar fin a +/- 1,3 m/s. Per las chartas davent d`ina autezza da 100m sur il terren stattan a disposiziun marcantamain main mesiraziuns per la modellaziun. Uschia resulta ina intschertezza pli gronda dals resultats. Las indicaziuns ston vegnir chapidas sco valitaziun approximativa da las relaziuns da vent. Sch`in interess per il svilup d`in tschert lieu è avant maun, ston vegnir fatgas mesiraziuns al lieu.</Abstract>
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        <Title>Implants d`energia dal vent</Title>
        <Abstract>Tar implants d`energia dal vent lascha l`energia chinetica da l`aria affluenta rotar las alas da l`implant. L`energia mecanica che vegn producida uschia vegn transfurmada d`in generatur en energia electrica. L`emprim implant d`energia dal vent da la Svizra è vegnì mess en funcziun l`onn 1986 a Soolhof (Langenbruck, BL). El aveva ina prestaziun da 28 kW. L`onn 2013 datti en tut 34 implants d`energia dal vent che produceschan circa 85 uras da gigawatt (GWh) electricitad cun la forza dal vent. Il parc eroelectric il pli grond sa chatta sin il Mont Crosin en il Giura bernais tar St. Imier: Qua stattan 16 turbinas da vent cun ina prestaziun totala da 23,6 MW. Ulteriurs implants gronds sa chattan tranter auter en la Val dal Rodan (VS), tar Entlebuch (LU) e sin il Gütsch sur Andermatt (UR). En Svizra po l`energia dal vent sa sviluppar anc fitg. Uschia duain implants d`energia dal vent producir fin l`onn 2020 circa 600 GWh e fin l`onn 2050 circa 4000 GWh electricitad per onn. Lieus adattads sa chattan sin las collinas dal Giura, ma er en las Alps ed en las Prealps ed en la Svizra bassa dal vest. Las geodatas spezialas `Implants d`energia dal vent` documenteschan l`effectiv actual d`implants d`energia dal vent da la Svizra. Tut las infurmaziuns sa basan sin las infurmaziuns dals gestiunaris dals implants. Las indicaziuns servan sco material d`infurmaziun per la publicitad e n`èn betg infurmaziuns uffizialas u explicaziuns giuridicamain liantas.</Abstract>
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        <Title>Implants da biogas</Title>
        <Abstract>En implants da biogas vegn producì gas cun agid da la fermentaziun da material organic. La maschaida da gas che resulta en quest connex consista per gronda part da metan (CH4) ritg d`energia e da dioxid carbonic (CO2). Biogas po vegnir duvrà per producir electricitad e chalur sco er sco carburant. En Svizra datti passa 100 implants da biogas. En cas da la producziun indigena da biogas vegnan elavurads exclusivamain ruments e vanzadiras da spaisas da chasadas, da l`industria da victualias e da l`agricultura. Pervia da quai n`è biogas betg mo in purtader d`energia regenerabel e neutral areguard il CO2, mabain er persistent. Cun biogas pon vegnir producidas directamain electricitad e chalur en ina centrala termoelectrica cumplessiva. Or da biogas po però er vegnir fatg biometan che po alura vegnir inducì en la rait da gas natiral. Quel stat alura puspè a disposiziun per la producziun d`electricitad e da chalur sco er sco carburant. Las geodatas davart implants da biogas infurmeschan davart il stadi actual da tals stabiliments per la producziun d`energia en Svizra. Actualmain sa basan las datas mo sin la glista dals retschaviders dad ICF. La finamira a lunga vista è quella da pudair registrar tut ils implants da biogas ch`èn en funcziun en Svizra - independentamain, sch`els produceschan electricitad u chalur en l`implant u sch`els induceschan biometan en la rait da gas natiral. Las datas èn destinadas per infurmar la vasta publicitad e n`èn betg indicaziuns uffizialas u liantas.</Abstract>
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      <Abstract>Il Concept energia da vent è in concept tenor l`art. 13 da la Lescha federala davart la planisaziun dal territori (LPT; CS 700). Il concept definescha d`ina vart ils interess federals ils pli impurtants che ston vegnir resguardads tar la planisaziun d`implants d`energia da vent, e da l`autra vart las zonas principalas da potenzial che ston vegnir scleridas en il rom da la planisaziun directiva chantunala. Tras quai augmenta il Concept energia da vent la segirezza da planisaziun. Las zonas principalas da potenzial èn vegnidas eruidas da la Confederaziun resguardond ils gronds retgavs d`energia da vent (datas da basa: Atlas dal vent da la Svizra, www.windatlas.ch), ils interess federals ils pli impurtants ed ina concentraziun spaziala suffizienta. L`analisa generala cuntegna malsegirezzas e na resguarda en quest connex nagins interess chantunals e communals e na permetta naginas explicaziuns davart la realisabladad concreta d`implants d`energia da vent. La preschentaziun cartografica da las zonas principalas da potenzial na represchenta pia betg ina planisaziun positiva da la Confederaziun. Ella na concurrenzescha naginas inscripziuns approvadas en il plan directiv e fa mo indicaziuns fin a la scala 1:50`000. Igl è chaussa dals chantuns da designar territoris adattads per l`utilisaziun dal vent sco funtauna d`energia sin basa da las ponderaziuns respectivas dals interess confurmas al stgalim. Las geodatas da las zonas principalas da potenzial n`han nagin caracter liant per las autoritads, mabain ston vegnir chapidas primarmain sco ina basa da la Confederaziun per ils chantuns che n`han en lur plan directiv anc nagin chapitel che tracta l`energia da vent u che vulan adattar in chapitel correspundent en lur plan directiv. La forza expressiva cumplaina da la charta sa fa valair pir, sch`ins resguarda las explicaziuns en il Concept energia da vent sco er en il rapport explicativ respectiv.</Abstract>
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        <Abstract>Il Concept energia da vent è in concept tenor l`art. 13 da la Lescha federala davart la planisaziun dal territori (LPT; CS 700). Il concept definescha d`ina vart ils interess federals ils pli impurtants che ston vegnir resguardads tar la planisaziun d`implants d`energia da vent, e da l`autra vart las zonas principalas da potenzial che ston vegnir scleridas en il rom da la planisaziun directiva chantunala. Tras quai augmenta il Concept energia da vent la segirezza da planisaziun. Las zonas principalas da potenzial èn vegnidas eruidas da la Confederaziun resguardond ils gronds retgavs d`energia da vent (datas da basa: Atlas dal vent da la Svizra, www.windatlas.ch), ils interess federals ils pli impurtants ed ina concentraziun spaziala suffizienta. L`analisa generala cuntegna malsegirezzas e na resguarda en quest connex nagins interess chantunals e communals e na permetta naginas explicaziuns davart la realisabladad concreta d`implants d`energia da vent. La preschentaziun cartografica da las zonas principalas da potenzial na represchenta pia betg ina planisaziun positiva da la Confederaziun. Ella na concurrenzescha naginas inscripziuns approvadas en il plan directiv e fa mo indicaziuns fin a la scala 1:50`000. Igl è chaussa dals chantuns da designar territoris adattads per l`utilisaziun dal vent sco funtauna d`energia sin basa da las ponderaziuns respectivas dals interess confurmas al stgalim. Las geodatas da las zonas principalas da potenzial n`han nagin caracter liant per las autoritads, mabain ston vegnir chapidas primarmain sco ina basa da la Confederaziun per ils chantuns che n`han en lur plan directiv anc nagin chapitel che tracta l`energia da vent u che vulan adattar in chapitel correspundent en lur plan directiv. La forza expressiva cumplaina da la charta sa fa valair pir, sch`ins resguarda las explicaziuns en il Concept energia da vent sco er en il rapport explicativ respectiv.</Abstract>
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        <Abstract>Il UFAC po fixar lingias da construcziun per segirar implants d`eroports existents u futurs. Las lingias da construcziun ston correspunder al stadi final probabel e tegnair quint da la planisaziun dal territori sco er da la protecziun da l`ambient. Ellas pon esser limitadas verticalmain. Entaifer las lingias da construcziun na dastgan vegnir fatgas naginas midadas architectonicas u ulteriuras intervenziuns che cuntrafan a l`intent da las lingias da construcziun. Exceptadas èn intervenziuns che servan al mantegniment u a l`allontanament da privels e d`influenzas nuschaivlas. Il UFAC n`ha fin ussa betg fatg diever da quest instrument. Perquai n`existan nagins cuntegns e nagin model da geodatas minimal tar questa unitad da datas. L`unitad da metadatas serva unicamain a descriver il feature service per il plaun respectiv en ils catasters RPDP chantunals.</Abstract>
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        <Abstract>En cas dals territoris surbajegiads tenor il dretg svizzer davart l`aviatica sa tracti d`ina definiziun quantitativa ed applitgabla en reguard a criteris aviatics da las surfatschas che vegnan applitgadas en ils art. 63 e 65a da l`Ordinaziun dals 23 da november 1994 davart l`infrastructura da l`aviatica (OIAv; CS 748.131.1). In`obligaziun da dumandar ina permissiun en il territori surbajegià ed en il territori betg surbajegià vala per objects d`ina autezza da 100m e dapli (per lingias d`auta tensiun, implants d`energia da vent e slacklines gia a partir da 60m e dapli) sco er tar objects che penetreschan ina surfatscha ch`è inscritta en in cataster da las surfatschas da limitaziun d`obstachels u en in plan da la zona da segirezza. In`obligaziun da registraziun vala per objects cun in`autezza da 60m e dapli en territoris surbajegiads e cun in`autezza da 25m e dapli en territoris betg surbajegiads (u en cas da cranas moviblas pir a partir d`ina autezza da 40m e dapli). Ils proprietaris ston laschar registrar ad ura dal UFAC quests edifizis e quests stabiliments u objects temporars avant che construir u midar tals. Questa unitad da datas vectorialas per la Svizra e per il Principadi da Liechtenstein vegn generada automaticamain or dals plans d`edifizis dal product `swissTLM3D` da swisstopo ed actualisada periodicamain.</Abstract>
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      <Abstract>En cas da las datas dals obstachels da l`aviatica sa tracti da datas tenor l`art. 2 lit. k da l`Ordinaziun dals 23 da november 1994 davart l`infrastructura da l`aviatica (OIAv; CS 748.131.1). Obstachels da l`aviatica èn edifizis e stabiliments (tranter auter antennas, edifizis, cabels, cranas, pendicularas, lingias d`auta tensiun, implants d`energia da vent) sco er plantas che pon difficultar, periclitar u impedir il manaschi d`eromobils u d`implants da controlla dal traffic aviatic. Els vegnan registrads en il rom da l`obligaziun da dumandar ina permissiun tenor l`art. 63 OIAv resp. en il rom da l`obligaziun da registraziun tenor l`art. 65a OIAv. L`unitad da datas qua avant maun cuntegna - cun excepziun da las plantas - tut ils obstachels da l`aviatica permanents e temporars, sch`els cuntanschan en territoris betg surbajegiads in`autezza da 25 meters e dapli (en cas da cranas moviblas 40 meters e dapli) u sch`els cuntanschan en territoris surbajegiads in`autezza d`almain 60 meters.</Abstract>
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        <Abstract>L`Atlas a bindel lartg dat ina survista dal provediment cun raits da telecommunicaziun modernas en Svizra. La situaziun da provediment vegn preschentada en furma da datas statisticas pro quadrat da coordinatas (250x250 m). La charta mussa il dumber da gestiunaris pro quadrat da coordinatas che pon furnir servetschs ubain sur lur agens attatgs ubain sur prestaziuns preliminaras. Sch`ins clicca sin in quadrat da coordinatas, vegn mussada la glista da las societads. Sch`ins clicca lura sin il num da la societad, s`avra la pagina d`internet da quella. Là chattan ins infurmaziuns davart ils servetschs da telecommunicaziun da questa firma e/u da partenaris. Per tscherts lieus n`è la glista betg cumpletta. La situaziun da provediment effectiva po vegnir dumandada tar las societads.</Abstract>
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        <Abstract>L`Atlas a bindel lartg dat ina survista dal provediment cun raits da telecommunicaziun modernas en Svizra. La situaziun da provediment vegn preschentada en furma da datas statisticas pro quadrat da coordinatas (250x250 m). La charta mussa, en quants edifizis ch`i vegn purschì ina sveltezza da download da l`internet dad 10 Mbit/s u dapli sur la rait fixa (en pertschient da las entradas d`edifizis per utilisaziun abitativa u commerziala tenor l`Uffizi federal da statistica). La situaziun da provediment vegn preschentada senza garanzia. La situaziun da provediment effectiva po vegnir dumandada tar las societads. Vesair en quest reguard l`infurmaziun supplementara tar la charta &#39;Societads cun atgna rait&#39;.</Abstract>
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        <Abstract>L`Atlas a bindel lartg dat ina survista dal provediment cun raits da telecommunicaziun modernas en Svizra. La situaziun da provediment vegn preschentada en furma da datas statisticas pro quadrat da coordinatas (250x250 m). La charta mussa, en quants edifizis ch`i vegn purschì ina sveltezza da download da l`internet dad 300 Mbit/s u dapli sur la rait fixa (en pertschient da las entradas d`edifizis per utilisaziun abitativa u commerziala tenor l`Uffizi federal da statistica). La situaziun da provediment vegn preschentada senza garanzia. La situaziun da provediment effectiva po vegnir dumandada tar las societads. Vesair en quest reguard l`infurmaziun supplementara tar la charta &#39;Societads cun atgna rait&#39;.</Abstract>
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        <Abstract>L`Atlas a bindel lartg dat ina survista dal provediment cun raits da telecommunicaziun modernas en Svizra. La situaziun da las raits da communicaziun mobila è preschentada en furma da quadrats da coordinatas (100x100 meters). Per mintga quadrat da coordinatas mussa la carta il dumber da gestiunaris che porschan teoreticamain ina colliaziun 3G, sch`ins sa chatta en il liber (sin via, sin ina plazza publica e.u.v.). Il provediment preschentà sin la carta è ina cumpilaziun da las datas furnidas da tut ils gestiunaris da raits da communicaziun mobila. Tut las indicaziuns èn senza garanzia. Davart la situaziun effectiva dal provediment pon ins s`infurmar directamain tar ils purschiders: &lt;a href=&#39;https://www.salt.ch/en/mobile/coverage&#39;&gt;Salt&lt;/a&gt;, &lt;a href=&#39;https://sunrise.mapplus.ch/&#39;&gt;Sunrise UPC&lt;/a&gt;, &lt;a href=&#39;https://scmplc.begasoft.ch/plcapp/pages/gis/netzabdeckung.jsf&#39;&gt;Swisscom&lt;/a&gt;</Abstract>
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        <Abstract>L`Atlas a bindel lartg dat ina survista dal provediment cun raits da telecommunicaziun modernas en Svizra. La situaziun da las raits da communicaziun mobila è preschentada en furma da quadrats da coordinatas (100x100 meters). Per mintga quadrat da coordinatas mussa la carta il dumber da gestiunaris che porschan teoreticamain ina colliaziun 4G, sch`ins sa chatta en il liber (sin via, sin ina plazza publica e.u.v.). Il provediment preschentà sin la carta è ina cumpilaziun da las datas furnidas da tut ils gestiunaris da raits da communicaziun mobila. Tut las indicaziuns èn senza garanzia. Davart la situaziun effectiva dal provediment pon ins s`infurmar directamain tar ils purschiders: &lt;a href=&#39;https://www.salt.ch/en/mobile/coverage&#39;&gt;Salt&lt;/a&gt;, &lt;a href=&#39;https://sunrise.mapplus.ch/&#39;&gt;Sunrise UPC&lt;/a&gt;, &lt;a href=&#39;https://scmplc.begasoft.ch/plcapp/pages/gis/netzabdeckung.jsf&#39;&gt;Swisscom&lt;/a&gt;</Abstract>
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        <Abstract>L`Atlas a bindel lartg dat ina survista dal provediment cun raits da telecommunicaziun modernas en Svizra. La situaziun da las raits da communicaziun mobila è preschentada en furma da quadrats da coordinatas (100x100 meters). Per mintga quadrat da coordinatas mussa la carta il dumber da gestiunaris che porschan teoreticamain ina colliaziun 5G, sch`ins sa chatta en il liber (sin via, sin ina plazza publica e.u.v.). Il provediment preschentà sin la carta è ina cumpilaziun da las datas furnidas da tut ils gestiunaris da raits da communicaziun mobila. Tut las indicaziuns èn senza garanzia. Davart la situaziun effectiva dal provediment pon ins s`infurmar directamain tar ils purschiders: &lt;a href=&#39;https://www.salt.ch/en/mobile/coverage&#39;&gt;Salt&lt;/a&gt;, &lt;a href=&#39;https://sunrise.mapplus.ch/&#39;&gt;Sunrise UPC&lt;/a&gt;, &lt;a href=&#39;https://scmplc.begasoft.ch/plcapp/pages/gis/netzabdeckung.jsf&#39;&gt;Swisscom&lt;/a&gt;</Abstract>
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        <Abstract>Dad in clom d`urgenza sa tracti, sch`ina persuna cumpona in numer curt da trais cifras dal servetsch da clom d`urgenza: numer d`urgenza europeic 112; polizia 117; pumpiers 118; sguard da victima 142; maun offert 143; alarm sanitar 144; agid al telefon per uffants e giuvenils 147. In clom d`urgenza po succeder sur ina rait fixa, sur ina rait per telefonia mobila u sur ina rait da satellit. La chiamata d`emergenza deve essere istradata verso la centrale d`allarme del servizio locale competente per il caso specifico. Una regione in cui le chiamate d`emergenza vengono istradate verso una determinata centrale d`allarme costituisce una zona d`intervento. La carta mostra la posizione de centrale d`allarme per le chiamate d`emergenza 147 effettuate dalla rete fissa, mobile o via satellite. Per ciascuna zona d`intervento si può identificare le centrale d`allarme 147 e numero di routing selezionando la zona desiderata. Les centrales d`alarme 147 fixe,mobile et par satellite de la zone desservie peuvent être une même centrale ou des centrales différentes.</Abstract>
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        <Abstract>L`Atlas a bindel lartg dat ina survista dal provediment cun raits da telecommunicaziun modernas en Svizra. La situaziun da provediment vegn preschentada en furma da datas statisticas pro quadrat da coordinatas (250x250 m). La charta mussa, en quants edifizis ch`i vegn purschì ina sveltezza dad upload da l`internet dad 1 Mbit/s u dapli sur la rait fixa (en pertschient da las entradas d`edifizis per utilisaziun abitativa u commerziala tenor l`Uffizi federal da statistica). La situaziun da provediment vegn preschentada senza garanzia. La situaziun da provediment effectiva po vegnir dumandada tar las societads. Vesair en quest reguard l`infurmaziun supplementara tar la charta &#39;Societads cun atgna rait&#39;.</Abstract>
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        <Abstract>L`Atlas a bindel lartg dat ina survista dal provediment cun raits da telecommunicaziun modernas en Svizra. La situaziun da provediment vegn preschentada en furma da datas statisticas pro quadrat da coordinatas (250x250 m). La charta mussa, en quants edifizis ch`i vegn purschì ina sveltezza dad upload da l`internet da 100 Mbit/s u dapli sur la rait fixa (en pertschient da las entradas d`edifizis per utilisaziun abitativa u commerziala tenor l`Uffizi federal da statistica). La situaziun da provediment vegn preschentada senza garanzia. La situaziun da provediment effectiva po vegnir dumandada tar las societads. Vesair en quest reguard l`infurmaziun supplementara tar la charta &#39;Societads cun atgna rait&#39;.</Abstract>
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        <Abstract>Dapi la mesadad dals onns 1950 èn las mortalitads dals amfibis sin via s`augmentadas drasticamain. Mintga onn traversan en Svizra tschientmillis amfibis vias sin lur migraziun tranter ils habitats rurals e las auas da fregar, e vegnan pia savens mazzads, sch`i na vegnan betg prendidas mesiras da protecziun. Quai n`è betg mo in problem da segirezza per il traffic, mabain chaschuna er reducziuns massivas da la populaziun dals amfibis. Las migraziuns entaifer las populaziuns han lieu sin las rutas da migraziun ch`èn pli u main adina las medemas. Las migraziuns han lieu durant tschertas stagiuns e permettan als amfibis da viver temporarmain en differents tips da habitats, ch`èn separads territorialmain in da l`auter. Per mantegnair las populaziuns èn questas migraziuns indispensablas. Info fauna karch maina ina banca da datas davart ils lieus, nua che las rutas da migraziun dals amfibis stattan en conflict cun l`infrastructura dal traffic. Actualmain èn enconuschents stgars 2000 lieus da conflict che vegnan numnads &#39;lieus da migraziun d`amfibis&#39; en la lingua tecnica. Tut tenor la grondezza da la populaziun d`amfibis, da l`intensitad dal traffic e da las pussaivladads al lieu vegnan realisadas mesiras da protecziun, sco p.ex. l`installaziun da tunnels e d`indrizs directivs per animals pitschens, saivs d`amfibis temporaras, bloccadas temporaras da vias u patruglias temporaras. Ils lieus da conflict enconuschents da las migraziuns d`amfibis en Svizra èn cuntegnids en questa unitad da geodatas e pon vegnir visualisads.</Abstract>
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        <Abstract>Ils territoris d`inundaziun d`Aquaprotect dattan ina survista approximativa, elavurada cun metodas simplas, dals territoris potenzialmain inundads a chaschun d`auas grondas raras e fitg raras en l`entira Svizra. Perquai ch`els dattan mo ina survista approximativa dals privels e da las ristgas, na remplazzan els betg las chartas da privel detagliadas (http://www.bafu.admin.ch/gefahrenkarten). Els na resguardan per exempel betg las mesiras existentas da la protecziun cunter aua gronda e permettan perquai mo da valitar en moda approximativa in`eventuala periclitaziun tras aua gronda en lieus, nua che chartas da privel mancan anc. Ils territoris d`inundaziun d`Aquaprotect èn avant maun per auas grondas cun frequenzas da 50, 100, 250 e 500 onns. In`aua gronda d`ina frequenza da per exempel 100 onns ha ina quantitad da deflussiun che vegn cuntanschida en media - guardà sur ina perioda fitg lunga - ina giada entaifer 100 onns. Dal fatg ch`in tschert territori n`è betg cuntegnì en ils territoris d`inundaziun d`Aquaprotect na dastgi betg vegnir concludì ch`i n`exista là nagin privel d`aua gronda. Pervia da la contemplaziun simplifitgada dattan las surfatschas inditgadas ina survista approximativa. En cas da scalas pli detagliadas che 1:50`000 vegnan ils territoris d`inundaziun represchentads mo pli cun agid da schraffuras. Uschia duain vegnir evitadas faussas interpretaziuns per ils territoris pertutgads resp. betg pertutgads en consequenza da represchentaziuns betg dal tuttafatg exactas.</Abstract>
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        <Abstract>Ils territoris d`inundaziun d`Aquaprotect dattan ina survista approximativa, elavurada cun metodas simplas, dals territoris potenzialmain inundads a chaschun d`auas grondas raras e fitg raras en l`entira Svizra. Perquai ch`els dattan mo ina survista approximativa dals privels e da las ristgas, na remplazzan els betg las chartas da privel detagliadas (http://www.bafu.admin.ch/gefahrenkarten). Els na resguardan per exempel betg las mesiras existentas da la protecziun cunter aua gronda e permettan perquai mo da valitar en moda approximativa in`eventuala periclitaziun tras aua gronda en lieus, nua che chartas da privel mancan anc. Ils territoris d`inundaziun d`Aquaprotect èn avant maun per auas grondas cun frequenzas da 50, 100, 250 e 500 onns. In`aua gronda d`ina frequenza da per exempel 100 onns ha ina quantitad da deflussiun che vegn cuntanschida en media - guardà sur ina perioda fitg lunga - ina giada entaifer 100 onns. Dal fatg ch`in tschert territori n`è betg cuntegnì en ils territoris d`inundaziun d`Aquaprotect na dastgi betg vegnir concludì ch`i n`exista là nagin privel d`aua gronda. Pervia da la contemplaziun simplifitgada dattan las surfatschas inditgadas ina survista approximativa. En cas da scalas pli detagliadas che 1:50`000 vegnan ils territoris d`inundaziun represchentads mo pli cun agid da schraffuras. Uschia duain vegnir evitadas faussas interpretaziuns per ils territoris pertutgads resp. betg pertutgads en consequenza da represchentaziuns betg dal tuttafatg exactas.</Abstract>
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        <Abstract>Per dar als chantuns la pussaivladad da prender per mauns uschè svelt sco pussaivel la protecziun da las zonas umidas d`impurtanza probablamain naziunala, ha il UFAGC laschà elavurar l`onn 1987 ina cartaziun detagliada da la vegetaziun dals objects da la versiun da consultaziun per mauns dals chantuns. Per ina gronda part dals objects ch`èn vegnids engrondids suenter la consultaziun, èn vegnidas fatgas posteriuramain cartas da la vegetaziun tenor la medema metoda. In dumber pli grond da quests novs objects da l`inventari sco er da tut ils objects ch`èn vegnids integrads en l`inventari en il rom da la 2. e 3. cumplettaziun sco er da la revisiun 2007 (senza zonas umidas alpinas) èn vegnids cartads tenor il medem sistem cun agid da fotografias fotogrammetricas ord l`aria a radis infracotschens.</Abstract>
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        <Abstract>La basa per elavurar las regiuns biogeograficas (en 6 u 12 classas) eran las surfatschas omogenas dals territoris d`intschess da flums. Sin questas surfatschas èn las infurmaziuns relevantas e suffizientamain cumplettas davart las spezias dals centers da datas infofauna, infoflora, staziun ornitologica e briofits vegnidas analisadas e classifitgadas tenor gruppas cun caracteristicas sumegliantas. Las datas faunisticas èn vegnidas elavuradas sin basa da la metoda Wohlgemuth (1996), la quala è vegnida sustegnida cun ulteriuras proceduras per calcular ils indexs da dissumeglientscha, cun matrizas da spezias e cun tests. Ina gronda part da las analisas è vegnida fatga cun agid da la &#39;Open Source Software R&#39;. Ils resultats èn vegnids preschentads en in emprim pass en sis gruppas ed alura en in segund pass en dudesch gruppas. Fin sin in pèr paucas excepziuns vegnivan ils cunfins furmads dals intschess da las auas. En paucs cas èn vegnids duvrads criteris topografics ed il cussegl d`expertas e d`experts.</Abstract>
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        <Abstract>En Svizra vivan oz 19 spezias d`amfibis - bunamain tuttas èn sin la Glista cotschna da las spezias d`animals periclitadas. La surfatscha da las zonas umidas sco biotop dals amfibis è sa reducida entaifer ils ultims 100 onns a main ch`in dieschavel. Ils biotops restants duessan perquai vegnir preservads. Sco quart inventari federal tenor l`art. 18a LPNP ha il Cussegl federal mess en vigur l`onn 2001 l`Inventari federal da las plazzas da fregar per amfibis cun 701 objects. Ils onns 2003, 2007, 2017 e 2025 è quel vegnì revedì. Actualmain èn en vigur 969 objects (873 objects fixs e 96 objects movibels). Plinavant cuntegna l`agiunta 3 tut en tut 25 objects, dals quals ils perimeters n`èn betg anc rectifitgads definitivamain. Fin ch`igl è decidì d`als integrar en l`agiunta 1 u 2, sa drizza lur protecziun tenor l`artitgel 29 alinea 1 litera a da l`Ordinaziun davart la protecziun da la natira e da la patria (OPNP) e tenor l`artitgel 10 da l`Ordinaziun davart la protecziun da las plazzas da fregar per amfibis d`impurtanza naziunala (OPFA).</Abstract>
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        <Abstract>Sco biotops natirals en il sectur d`inundaziun da las auas sa diminueschan las zonas umidas pli e pli. Il matg 1981 ha il DFI surdà a l`Institut federal da retschertgas forestalas (oz WSL) l`incumbensa d`elavurar in inventari scientific da las zonas umidas. Quest inventari è vegnì elavurà en l`institut da la gruppa per la perscrutaziun da la vegetaziun. Tenor l`art. 18a da la Lescha federala dal 1. da fanadur 1966 davart la protecziun da la natira e da la patria (LPNP) designescha il Cussegl federal ils biotops d`impurtanza naziunala, fixescha la situaziun da quests biotops e determinescha las finamiras da protecziun (art. 18a LPNP ch`è en vigur dapi il 1. da favrer 1988). Quai fa el suenter avair tadlà ils chantuns. Sco segund inventari federal tenor l`art. 18a LPNP ha il Cussegl federal mess en vigur l`onn 1992 l`Inventari federal da las zonas umidas cun 169 objects. Ils onns 2001, 2003 e 2007 hai dà trais cumplettaziuns. Ils onns 1995 fin 1997 è vegnì elavurà - sco inventari scientific - l`Inventari dals avantglatschers e da las planiras alluvialas alpinas (ITAPA) sco basa da l`emprima cumplettaziun. Actualmain èn en vigur 326 objects. Plinavant cuntegna l`agiunta 2 tut en tut 27 objects, dals quals ils perimeters n`èn betg anc rectifitgads definitivamain. Fin ch`igl è decidì d`als integrar en l`agiunta 1, sa drizza lur protecziun tenor l`artitgel 29 alinea 1 litera a da l`Ordinaziun davart la protecziun da la natira e da la patria (OPNP) e tenor l`artitgel 7 da l`Ordinaziun da las zonas umidas.</Abstract>
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        <Abstract>La finamira da la protecziun da biotops tenor l`art. 18a da la Lescha federala davart la protecziun da la natira e da la patria LPNP (CS 451) è ina protecziun efficazia da las surfatschas d`impurtanza naziunala dals tips da biotop ils pli impurtants. L`onn 1992 è vegni mess en vigur l`Inventari federal da las zonas umidas d`impurtanza naziunala (Inventari da las zonas umidas) che cuntegna 169 zonas umidas. Tranter 1995 e 1998 èn vegnids inventarisads ils avantglatschers e las planiras alluvialas alpinas da la Svizra. L`onn 2001 èn vegnids inscrits en l`Inventari da las zonas umidas 52 avantglatschers e 14 planiras alluvialas sco zonas umidas alpinas d`impurtanza naziunala. Ils onns 2003 fin 2005 è vegnì registrà pli detagliadamain il stadi da las zonas umidas alpinas da l`inventari. L`unitad da geodatas documentescha las datas nunelavuradas da la retschertga da la vegetaziun sco er las caracteristicas deducidas da tala per applicaziuns spezialas.</Abstract>
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        <Abstract>Las pastgiras ed ils prads sitgs èn resultads grazia a l`agricultura: Els èn il resultat d`ina cultivaziun extensiva durant blers tschientaners e d`ina agricultura tradiziunala. Dapi la fin dal 19avel tschientaner è l`effectiv da pastgiras e da prads sitgs sa reducì per circa 90 %. Parallelamain èn las spezias indigenas che vivan en quests biotops vegnidas adina pli fitg sut squitsch: Stgars 40 % da tut las spezias da plantas e 50 % da tut las spezias d`animals, che dovran lieus sitgs per viver, figureschan oz sin las glistas cotschnas naziunalas. Malgrà differents inventaris chantunals manca ina survista svizra dals biotops dals prads sitgs che pussibilitescha da metter prioritads per mesiras da mantegniment e per ina controlla dal success. Sco ultim inventari federal tenor l`art. 18a LPNP ha il Cussegl federal mess en vigur l`onn 2010 l`Inventari federal da las pastgiras e dals prads sitgs cun 2934 objects. Ils onns 2012, 2017, 2021 e 2025 è quel vegnì revedì. Actualmain èn en vigur 4083 objects. Plinavant cuntegna l`agiunta 2 tut en tut 38 objects dals quals ils perimeters n`èn betg anc rectifitgads definitivamain. Fin ch`igl è decidì d`als integrar en l`agiunta 1, sa drizza lur protecziun tenor l`artitgel 29 alinea 1 litera a da l`Ordinaziun davart la protecziun da la natira e da la patria (OPNP) e tenor l`artitgel 10 da l`Ordinaziun davart ils prads sitgs (OPPS).</Abstract>
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        <Abstract>Las pastgiras ed ils prads sitgs èn resultads grazia a l`agricultura: Els èn il resultat d`ina cultivaziun extensiva durant blers tschientaners e d`ina agricultura tradiziunala. Dapi la fin dal 19avel tschientaner è l`effectiv da pastgiras e da prads sitgs sa reducì per circa 90 %. Parallelamain èn las spezias indigenas che vivan en quests biotops vegnidas adina pli fitg sut squitsch: Stgars 40 % da tut las spezias da plantas e 50 % da tut las spezias d`animals, che dovran lieus sitgs per viver, figureschan oz sin las glistas cotschnas naziunalas. Malgrà differents inventaris chantunals manca ina survista svizra dals biotops dals prads sitgs che pussibilitescha da metter prioritads per mesiras da mantegniment e per ina controlla dal success. Sco ultim inventari federal tenor l`art. 18a LPNP ha il Cussegl federal mess en vigur l`onn 2010 l`Inventari federal da las pastgiras e dals prads sitgs cun 2934 objects. Ils onns 2012, 2017, 2021 e 2025 è quel vegnì revedì. Actualmain èn en vigur 4083 objects. Plinavant cuntegna l`agiunta 2 tut en tut 38 objects dals quals ils perimeters n`èn betg anc rectifitgads definitivamain. Fin ch`igl è decidì d`als integrar en l`agiunta 1, sa drizza lur protecziun tenor l`artitgel 29 alinea 1 litera a da l`Ordinaziun davart la protecziun da la natira e da la patria (OPNP) e tenor l`artitgel 10 da l`Ordinaziun davart ils prads sitgs (OPPS).</Abstract>
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        <Abstract>Charta da las ristgas d`erosiun mensilas per la pastgira permanenta svizra cun ina dissoluziun spaziala da 100 m. Las chartas mussan la media da l`erosiun en tonnas per hectara e per mais. Las nianzas verdas inditgeschan ina ristga d`erosiun pitschna, las nianzas melnas ina ristga d`erosiun mesauna e las nianzas cotschnas ina ristga d`erosiun gronda. La charta da las ristgas d`erosiun mensilas è vegnida calculada cun la Revised Universal Soil Loss Equation (RUSLE). Per questa applicaziun RUSLE è la dinamica mensila dals facturs erosivitad pervia da precipitaziuns (factur R) e cuvrida dal terren (factur C) vegnida resguardada sco suonda: A(mais)=R(mais)*K*C(mais)*L*S*P. En quest connex èn A(mais) la perdita da terren en tonnas per hectara e mais ed R(mais) e C(mais) il factur R mensil (MJ mm ha⁻¹ h⁻¹ mais⁻¹) e factur C (senza dimensiun). Ils ulteriurs facturs d`erosiun èn l`erodabilitad dal terren (factur K), la lunghezza da la spunda (factur L) e la pendenza da la spunda (factur S) sco er mesiras da protecziun (factur P). Ils facturs RUSLE èn vegnids adattads a las cundiziuns spezialas da l`ambient da la pastgira permanenta svizra. Il factur P è vegnì integrà sco constanta cun la valur 1 en la calculaziun, perquai ch`i mancan datas territorialas davart il management da las pastgiras e davart sia influenza sin l`erosiun dal terren.</Abstract>
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        <Abstract>Charta da las ristgas d`erosiun mensilas per la pastgira permanenta svizra cun ina dissoluziun spaziala da 100 m. Las chartas mussan la media da l`erosiun en tonnas per hectara e per mais. Las nianzas verdas inditgeschan ina ristga d`erosiun pitschna, las nianzas melnas ina ristga d`erosiun mesauna e las nianzas cotschnas ina ristga d`erosiun gronda. La charta da las ristgas d`erosiun mensilas è vegnida calculada cun la Revised Universal Soil Loss Equation (RUSLE). Per questa applicaziun RUSLE è la dinamica mensila dals facturs erosivitad pervia da precipitaziuns (factur R) e cuvrida dal terren (factur C) vegnida resguardada sco suonda: A(mais)=R(mais)*K*C(mais)*L*S*P. En quest connex èn A(mais) la perdita da terren en tonnas per hectara e mais ed R(mais) e C(mais) il factur R mensil (MJ mm ha⁻¹ h⁻¹ mais⁻¹) e factur C (senza dimensiun). Ils ulteriurs facturs d`erosiun èn l`erodabilitad dal terren (factur K), la lunghezza da la spunda (factur L) e la pendenza da la spunda (factur S) sco er mesiras da protecziun (factur P). Ils facturs RUSLE èn vegnids adattads a las cundiziuns spezialas da l`ambient da la pastgira permanenta svizra. Il factur P è vegnì integrà sco constanta cun la valur 1 en la calculaziun, perquai ch`i mancan datas territorialas davart il management da las pastgiras e davart sia influenza sin l`erosiun dal terren.</Abstract>
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        <Abstract>Charta da las ristgas d`erosiun mensilas per la pastgira permanenta svizra cun ina dissoluziun spaziala da 100 m. Las chartas mussan la media da l`erosiun en tonnas per hectara e per mais. Las nianzas verdas inditgeschan ina ristga d`erosiun pitschna, las nianzas melnas ina ristga d`erosiun mesauna e las nianzas cotschnas ina ristga d`erosiun gronda. La charta da las ristgas d`erosiun mensilas è vegnida calculada cun la Revised Universal Soil Loss Equation (RUSLE). Per questa applicaziun RUSLE è la dinamica mensila dals facturs erosivitad pervia da precipitaziuns (factur R) e cuvrida dal terren (factur C) vegnida resguardada sco suonda: A(mais)=R(mais)*K*C(mais)*L*S*P. En quest connex èn A(mais) la perdita da terren en tonnas per hectara e mais ed R(mais) e C(mais) il factur R mensil (MJ mm ha⁻¹ h⁻¹ mais⁻¹) e factur C (senza dimensiun). Ils ulteriurs facturs d`erosiun èn l`erodabilitad dal terren (factur K), la lunghezza da la spunda (factur L) e la pendenza da la spunda (factur S) sco er mesiras da protecziun (factur P). Ils facturs RUSLE èn vegnids adattads a las cundiziuns spezialas da l`ambient da la pastgira permanenta svizra. Il factur P è vegnì integrà sco constanta cun la valur 1 en la calculaziun, perquai ch`i mancan datas territorialas davart il management da las pastgiras e davart sia influenza sin l`erosiun dal terren.</Abstract>
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        <Abstract>Charta da las ristgas d`erosiun mensilas per la pastgira permanenta svizra cun ina dissoluziun spaziala da 100 m. Las chartas mussan la media da l`erosiun en tonnas per hectara e per mais. Las nianzas verdas inditgeschan ina ristga d`erosiun pitschna, las nianzas melnas ina ristga d`erosiun mesauna e las nianzas cotschnas ina ristga d`erosiun gronda. La charta da las ristgas d`erosiun mensilas è vegnida calculada cun la Revised Universal Soil Loss Equation (RUSLE). Per questa applicaziun RUSLE è la dinamica mensila dals facturs erosivitad pervia da precipitaziuns (factur R) e cuvrida dal terren (factur C) vegnida resguardada sco suonda: A(mais)=R(mais)*K*C(mais)*L*S*P. En quest connex èn A(mais) la perdita da terren en tonnas per hectara e mais ed R(mais) e C(mais) il factur R mensil (MJ mm ha⁻¹ h⁻¹ mais⁻¹) e factur C (senza dimensiun). Ils ulteriurs facturs d`erosiun èn l`erodabilitad dal terren (factur K), la lunghezza da la spunda (factur L) e la pendenza da la spunda (factur S) sco er mesiras da protecziun (factur P). Ils facturs RUSLE èn vegnids adattads a las cundiziuns spezialas da l`ambient da la pastgira permanenta svizra. Il factur P è vegnì integrà sco constanta cun la valur 1 en la calculaziun, perquai ch`i mancan datas territorialas davart il management da las pastgiras e davart sia influenza sin l`erosiun dal terren.</Abstract>
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        <Abstract>Charta da las ristgas d`erosiun mensilas per la pastgira permanenta svizra cun ina dissoluziun spaziala da 100 m. Las chartas mussan la media da l`erosiun en tonnas per hectara e per mais. Las nianzas verdas inditgeschan ina ristga d`erosiun pitschna, las nianzas melnas ina ristga d`erosiun mesauna e las nianzas cotschnas ina ristga d`erosiun gronda. La charta da las ristgas d`erosiun mensilas è vegnida calculada cun la Revised Universal Soil Loss Equation (RUSLE). Per questa applicaziun RUSLE è la dinamica mensila dals facturs erosivitad pervia da precipitaziuns (factur R) e cuvrida dal terren (factur C) vegnida resguardada sco suonda: A(mais)=R(mais)*K*C(mais)*L*S*P. En quest connex èn A(mais) la perdita da terren en tonnas per hectara e mais ed R(mais) e C(mais) il factur R mensil (MJ mm ha⁻¹ h⁻¹ mais⁻¹) e factur C (senza dimensiun). Ils ulteriurs facturs d`erosiun èn l`erodabilitad dal terren (factur K), la lunghezza da la spunda (factur L) e la pendenza da la spunda (factur S) sco er mesiras da protecziun (factur P). Ils facturs RUSLE èn vegnids adattads a las cundiziuns spezialas da l`ambient da la pastgira permanenta svizra. Il factur P è vegnì integrà sco constanta cun la valur 1 en la calculaziun, perquai ch`i mancan datas territorialas davart il management da las pastgiras e davart sia influenza sin l`erosiun dal terren.</Abstract>
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        <Abstract>Charta da las ristgas d`erosiun mensilas per la pastgira permanenta svizra cun ina dissoluziun spaziala da 100 m. Las chartas mussan la media da l`erosiun en tonnas per hectara e per mais. Las nianzas verdas inditgeschan ina ristga d`erosiun pitschna, las nianzas melnas ina ristga d`erosiun mesauna e las nianzas cotschnas ina ristga d`erosiun gronda. La charta da las ristgas d`erosiun mensilas è vegnida calculada cun la Revised Universal Soil Loss Equation (RUSLE). Per questa applicaziun RUSLE è la dinamica mensila dals facturs erosivitad pervia da precipitaziuns (factur R) e cuvrida dal terren (factur C) vegnida resguardada sco suonda: A(mais)=R(mais)*K*C(mais)*L*S*P. En quest connex èn A(mais) la perdita da terren en tonnas per hectara e mais ed R(mais) e C(mais) il factur R mensil (MJ mm ha⁻¹ h⁻¹ mais⁻¹) e factur C (senza dimensiun). Ils ulteriurs facturs d`erosiun èn l`erodabilitad dal terren (factur K), la lunghezza da la spunda (factur L) e la pendenza da la spunda (factur S) sco er mesiras da protecziun (factur P). Ils facturs RUSLE èn vegnids adattads a las cundiziuns spezialas da l`ambient da la pastgira permanenta svizra. Il factur P è vegnì integrà sco constanta cun la valur 1 en la calculaziun, perquai ch`i mancan datas territorialas davart il management da las pastgiras e davart sia influenza sin l`erosiun dal terren.</Abstract>
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        <Abstract>Charta da las ristgas d`erosiun mensilas per la pastgira permanenta svizra cun ina dissoluziun spaziala da 100 m. Las chartas mussan la media da l`erosiun en tonnas per hectara e per mais. Las nianzas verdas inditgeschan ina ristga d`erosiun pitschna, las nianzas melnas ina ristga d`erosiun mesauna e las nianzas cotschnas ina ristga d`erosiun gronda. La charta da las ristgas d`erosiun mensilas è vegnida calculada cun la Revised Universal Soil Loss Equation (RUSLE). Per questa applicaziun RUSLE è la dinamica mensila dals facturs erosivitad pervia da precipitaziuns (factur R) e cuvrida dal terren (factur C) vegnida resguardada sco suonda: A(mais)=R(mais)*K*C(mais)*L*S*P. En quest connex èn A(mais) la perdita da terren en tonnas per hectara e mais ed R(mais) e C(mais) il factur R mensil (MJ mm ha⁻¹ h⁻¹ mais⁻¹) e factur C (senza dimensiun). Ils ulteriurs facturs d`erosiun èn l`erodabilitad dal terren (factur K), la lunghezza da la spunda (factur L) e la pendenza da la spunda (factur S) sco er mesiras da protecziun (factur P). Ils facturs RUSLE èn vegnids adattads a las cundiziuns spezialas da l`ambient da la pastgira permanenta svizra. Il factur P è vegnì integrà sco constanta cun la valur 1 en la calculaziun, perquai ch`i mancan datas territorialas davart il management da las pastgiras e davart sia influenza sin l`erosiun dal terren.</Abstract>
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        <Abstract>Ina banca da datas per registrar en l`entira Svizra ils volumens da gera transportads en las auas. Suenter ils eveniments devastants da la stad 1987, che han chaschunà gronds donns en bleras regiuns da la Svizra, ha la Gruppa da lavur per idrologia operaziunala (GHO) proponì da manar ina banca da datas per registrar ils volumens da gera. Per la banca da datas Solid collavura il UFAM cun ils chantuns e cun instituts da perscrutaziun. Quels furneschan las valurs da las quantitads da gera transportadas ch`èn vegnidas depositadas en ils collecturs da gera. Las quantitads vegnan stimadas cun agid d`instruments da mesiraziun u a chaschun da la svidada dals collecturs da gera. La banca da datas Solid cumpiglia ca. 100 collecturs da gera.</Abstract>
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        <Abstract>L`unitad da datas davart las populaziuns da litschalas d`impurtanza naziunala cumpiglia quatter products parzials (territori da derasaziun, zonas centralas, plazzas da fregar, habitats da larvas). Il layer &#39;Plazzas da fregar&#39; cuntegna ils trajects, en ils quals ha lieu la reproducziun natirala. Las datas da basa derivan da l`Atlas da derasaziun dals peschs e ciclostoms da la Svizra (Pedroli et al. 1991), da las statisticas chantunalas da pestga sco er dad infurmaziuns da las administraziuns chantunalas da pestga.</Abstract>
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        <Abstract>L`unitad da datas davart las populaziuns da litschalas d`impurtanza naziunala cumpiglia quatter products parzials (territori da derasaziun, zonas centralas, plazzas da fregar, habitats da larvas). Il layer &#39;Territori da derasaziun&#39; cuntegna ils trajects d`auas da 20 populaziuns da litschalas d`impurtanza naziunala. Las datas da basa derivan da l`Atlas da derasaziun dals peschs e ciclostoms da la Svizra (Pedroli et al. 1991), da las statisticas chantunalas da pestga sco er dad infurmaziuns da las administraziuns chantunalas da pestga.</Abstract>
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        <Abstract>L`unitad da datas cumpiglia las coordinatas da las plazzas da fregar en Svizra (ca. 100 lieus) sco er la media dal dumber d`animals activs en mintga plazza da fregar (media da 10 onns). Ils onns 1995 fin 2004 ha il UFAM fatg in monitoring naziunal dal nas en collavuraziun cun ils posts spezialisads chantunals per la pestga. Intent: Registrar il potenzial da reproducziun d`ina spezia da peschs ch`è fermamain periclitada e ch`è protegida en l`entira Europa tras la Convenziun da Berna.</Abstract>
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        <Abstract>La glista infurmescha en tge auas che la malsogna da peschs MRP (malsogna renala proliferativa) ha pudì vegnir cumprovada. La diagnosa sa basa sin la cumprova dal scherm en il preparat (tagl) istologic (fatga al Center per medischina da peschs e selvaschina). La glista mussa il stadi da savida davart la derasaziun da la malsogna.</Abstract>
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        <Abstract>L`Inventari dals pastgets flottants da la Svizra cuntegna 83 objects da pastgets flottants primars da caracter da palì transiziunala e da palì auta che han ina tscherta grondezza minimala. L`inventari è in`ulteriura specificaziun da l`Inventari da las palids autas e transiziunalas resp. da l`Inventari da las palids planivas e resguarda meglier ils pastgets flottants ch`èn per il solit main extendids. I sa tracta da pastgets cun bler chagliom d`in unic toc ch`èn situads sin in fundament impregnà d`aua u che flotteschan sin l`aua e che oscilleschan cleramain, sch`ins passa sin els. Ils objects èn vegnids generads sco coverage da puncts tras l`utilisaziun da las coordinatas da lur center (coordinatas naziunalas) che derivan da la banca da datas.</Abstract>
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        <Abstract>Ils onns 1967 fin 1979 è l`entira Svizra vegnida cartografada per la lavur vi da l`Atlas da derasaziun dals feleschs e fanerogams. Per quest intent è ella vegnida dividida en 593 surfatschas irregularas tenor aspects topografics. Ins ha differenzià 350 surfatschas da vallada, 215 surfatschas da muntogna e 28 surfatschas da lai. Sco cunfin tranter las surfatschas da vallada e da muntogna è vegnì tschernì en la gronda part dals cas il cunfin natiral dal guaud.</Abstract>
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        <Abstract>La numeraziun dals flums tenor Strahler inditgescha il grad da la diromaziun d`ina rait d`auas. Ella è la basa per analisas e descripziuns morfologicas d`ina aua. --- Tenor Strahler han las funtaunas il numer 1. Sche dus affluents dal medem numer d`ordinaziun s`uneschan, s`augmenta il numer d`ordinaziun per 1. Il Rain e l`Aara han il numer d`ordinaziun 9, il Rodan il numer d`ordinaziun 7. --- La numeraziun dals flums è vegnida calculada sin basa da la rait d`auas VECTOR25 GWN.</Abstract>
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        <Title>Charta periclit. defl. auas surf.</Title>
        <Abstract>Ils territoris d`inundaziun preschentads en la charta da periclitaziun da deflussiuns d`auas da surfatscha èn vegnids registrads en tut la Svizra ed il Liechtenstein tenor ina metoda unitara. Questa metoda sa basa sin ina modellaziun senza verificaziun u plausibilisaziun en la cuntrada. Uschia vegnan designads quels territoris ch`èn pertutgads potenzialmain en cas d`eveniments rars fin fitg rars. Qua tras vegn dada ina survista generala approximativa davart la periclitaziun tras ina deflussiun d`ina aua da surfatscha. I na vegnan betg designads quels territoris ch`èn pertutgads d`inundaziuns tras auas currentas ed i na vegnan resguardadas naginas ovras da protecziun u sutpassadis u passadis d`aua en scarpas da la viafier (uschia vegnan preschentadas p.ex. scarpas da las VFF en il MDT sco scarpas serradas senza passadis d`aua). Questa charta permetta da valitar approximativamain la periclitaziun tras deflussiuns d`auas da surfatscha, sch`i n`è betg avant maun ina charta da privels detagliada. La frequenza supponida è pli gronda che 100 onns, quai vul dir ch`in tal eveniment vegn a capitar a lunga vista en media ina giada en 100 onns. I n`è betg d`excluder ch`i dat deflussiuns d`auas da surfatscha er sin surfatschas ch`èn registradas en la charta sco betg pertutgadas. Questa charta na dastga betg vegnir duvrada en ina scala ch`è pli detagliada che 1:12`500 (Liechtenstein: 1:10`000) , per evitar sbagls en l`interpretaziun da territoris pertutgads e da territoris betg pertutgads. La charta n`ha nagina vigur giuridica lianta, ma ils chantuns èn libers da la surpigliar en lur basas davart ils privels sco charta d`infurmaziun da privels e da la publitgar en il geoportal chantunal.</Abstract>
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        <Abstract>La classa da sulom è ina indicaziun necessaria per determinar ils effects d`in terratrembel sin in edifizi tenor la norma da construcziun SIA 261. Las chartas da las classas da sulom sun da resguardar sco chartas d`infurmaziun e nun as referischan sün la singula parcella. En cas da malsegirezzas vegn la classa da sulom cartada metodicamain da la vart segira. Las chartas èn primarmain nizzaivlas en il rom d`examinaziuns preliminaras. Tar planisaziun da projects da construcziun sto la plausibilitad da la classa da sulom* vegnir verifitgada sin basa da scleriments locals. En cas da divergenzas motivadas duai vegnir duvrada la classa da sulom che sa basa sin las examinaziuns localas. Las chartas da las classas da sulom seismicas vegnan fatgas ed actualisadas dals chantuns sin atgna iniziativa sin basa dal mussavia metodic dal UFAM. En enclegientscha cun ils chantuns pertutgads metta il UFAM a disposiziun questas datas en moda centrala. Eventualas dumondas da correctura e remartgas ston vegnir drizzadas als chantuns respectivs, cun excepziun da la citad da Berna e da la Val dal Rain Songagliaisa (chartas da pilot dal UFAM). * La gronda part da las chartas sa basa sin la descripziun da las classas da sulom da la norma SIA 261, ediziun 2003. Questa descripziun è vegnida adattada l`onn 2014. Las differenzas tar la descripziun da las classas da sulom da la norma SIA 261:2020 ch`è actualmain en vigur e tar l`ediziun 2003 ston perquai vegnir resguardadas. La norma da referenza per la cartaziun (SIA 261:2003 u SIA 261:2020) è avant maun en l`infurmaziun davart l`object.</Abstract>
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        <Abstract>CCharta da las zonas da terratrembels tenor la norma da construcziun SIA 261 &#39;Effects per las structuras purtantas&#39; (2020). A mintga zona è dada ina valur da calculaziun da l`acceleraziun orizontala dal terren agd (en m/s2). Questa valur da calculaziun vegn duvrada per las dimensiuns seismicas da structuras purtantas tenor las normas da la SIA per structuras purtantas.</Abstract>
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        <Abstract>ECOS09 è il catalog dals terratrembels en Svizra ed a l`exteriur vischin. El cuntegna las suandantas funtaunas: - Catalog macroseismic da terratrembels en Svizra (MECOS 02) cun eveniments dapi l`onn 250 s.C. - annuaris da la Cumissiun svizra da terratrembels dapi l`onn 1879 - localisaziuns da terratrembels da la rait instrumentala dal Servetsch seismologic svizzer (SSS) dapi l`onn 1975 - cumplettaziuns da 12 catalogs da terratrembels da pajais vischins e d`agenturas internaziunalas. Questa unitad da datas mussa ina selecziun da terratrembels dal catalog ECOS09 ch`èn vegnids localisads en Svizra e che han cuntanschì ina intensitad dad almain VI (donns levs vi d`edifizis).</Abstract>
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        <Abstract>Cuntegna las mesiras preventivas actualas dals chantuns en connex cun il privel d`incendis da guaud</Abstract>
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        <Abstract>Concentraziuns d`elements interpoladas (mg/kg terra fina) en las stresas superiuras (0-20 cm) da la Svizra. Per las interpolaziuns d`Ordinary Kriging (1 km x 1 km) èn vegnidas resguardadas las datas da mesiraziuns da tut en tut 1201 lieus dal Monitoring da la biodiversitad en Svizra (MBD), da l`Observatori naziunal dal terren (NABO) e da l`Atlas da terren geochemic europeic (GEMAS). Las concentraziuns d`elements èn vegnidas analisadas en cumpariziuns d`aua roiala (HNO3:HCl:H2O) da provas da terren setgentadas (40 °C), crivladas (&lt; 2 mm) e silsuenter mieutas, quai cun agid da la spectrometria da massa cun plasma collià en moda inductiva. Lieus, nua che la surtratga antropogena da las concentraziuns d`elements era enconuschenta (funtaunas da puncts), èn vegnids exclus ordavant. Tar ils resultats da l`Atlas da terren geochemic sa tracti d`ina situaziun mumentana da las concentraziuns d`elements en las stresas superiuras da la Svizra (perioda da las emprovas: 2011-2015). Las chartas interpoladas servan a visualisar meglier regiuns cun concentraziuns augmentadas resp. bassas. I na pon dentant vegnir deducidas naginas infurmaziuns per singulas parcellas u conclusiuns definitivas a la geologia, a la biodisponibilitad, a la repartiziun procentuala da las funtaunas geogenas ed antropogenas u a la concentraziun dal terren. Citat: J. E. Reusser, M. B. Siegenthaler, L. H. E. Winkel, D. Wächter, R. Kretzschmar, R. G. Meuli: Geochemischer Bodenatlas der Schweiz. Agroscope, Zürich, 2023.</Abstract>
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        <Abstract>Concentraziuns d`elements interpoladas (mg/kg terra fina) en las stresas superiuras (0-20 cm) da la Svizra. Per las interpolaziuns d`Ordinary Kriging (1 km x 1 km) èn vegnidas resguardadas las datas da mesiraziuns da tut en tut 1201 lieus dal Monitoring da la biodiversitad en Svizra (MBD), da l`Observatori naziunal dal terren (NABO) e da l`Atlas da terren geochemic europeic (GEMAS). Las concentraziuns d`elements èn vegnidas analisadas en cumpariziuns d`aua roiala (HNO3:HCl:H2O) da provas da terren setgentadas (40 °C), crivladas (&lt; 2 mm) e silsuenter mieutas, quai cun agid da la spectrometria da massa cun plasma collià en moda inductiva. Lieus, nua che la surtratga antropogena da las concentraziuns d`elements era enconuschenta (funtaunas da puncts), èn vegnids exclus ordavant. Tar ils resultats da l`Atlas da terren geochemic sa tracti d`ina situaziun mumentana da las concentraziuns d`elements en las stresas superiuras da la Svizra (perioda da las emprovas: 2011-2015). Las chartas interpoladas servan a visualisar meglier regiuns cun concentraziuns augmentadas resp. bassas. I na pon dentant vegnir deducidas naginas infurmaziuns per singulas parcellas u conclusiuns definitivas a la geologia, a la biodisponibilitad, a la repartiziun procentuala da las funtaunas geogenas ed antropogenas u a la concentraziun dal terren. Citat: J. E. Reusser, M. B. Siegenthaler, L. H. E. Winkel, D. Wächter, R. Kretzschmar, R. G. Meuli: Geochemischer Bodenatlas der Schweiz. Agroscope, Zürich, 2023.</Abstract>
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        <Abstract>Concentraziuns d`elements interpoladas (mg/kg terra fina) en las stresas superiuras (0-20 cm) da la Svizra. Per las interpolaziuns d`Ordinary Kriging (1 km x 1 km) èn vegnidas resguardadas las datas da mesiraziuns da tut en tut 1201 lieus dal Monitoring da la biodiversitad en Svizra (MBD), da l`Observatori naziunal dal terren (NABO) e da l`Atlas da terren geochemic europeic (GEMAS). Las concentraziuns d`elements èn vegnidas analisadas en cumpariziuns d`aua roiala (HNO3:HCl:H2O) da provas da terren setgentadas (40 °C), crivladas (&lt; 2 mm) e silsuenter mieutas, quai cun agid da la spectrometria da massa cun plasma collià en moda inductiva. Lieus, nua che la surtratga antropogena da las concentraziuns d`elements era enconuschenta (funtaunas da puncts), èn vegnids exclus ordavant. Tar ils resultats da l`Atlas da terren geochemic sa tracti d`ina situaziun mumentana da las concentraziuns d`elements en las stresas superiuras da la Svizra (perioda da las emprovas: 2011-2015). Las chartas interpoladas servan a visualisar meglier regiuns cun concentraziuns augmentadas resp. bassas. I na pon dentant vegnir deducidas naginas infurmaziuns per singulas parcellas u conclusiuns definitivas a la geologia, a la biodisponibilitad, a la repartiziun procentuala da las funtaunas geogenas ed antropogenas u a la concentraziun dal terren. Citat: J. E. Reusser, M. B. Siegenthaler, L. H. E. Winkel, D. Wächter, R. Kretzschmar, R. G. Meuli: Geochemischer Bodenatlas der Schweiz. Agroscope, Zürich, 2023.</Abstract>
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        <Abstract>Concentraziuns d`elements interpoladas (mg/kg terra fina) en las stresas superiuras (0-20 cm) da la Svizra. Per las interpolaziuns d`Ordinary Kriging (1 km x 1 km) èn vegnidas resguardadas las datas da mesiraziuns da tut en tut 1201 lieus dal Monitoring da la biodiversitad en Svizra (MBD), da l`Observatori naziunal dal terren (NABO) e da l`Atlas da terren geochemic europeic (GEMAS). Las concentraziuns d`elements èn vegnidas analisadas en cumpariziuns d`aua roiala (HNO3:HCl:H2O) da provas da terren setgentadas (40 °C), crivladas (&lt; 2 mm) e silsuenter mieutas, quai cun agid da la spectrometria da massa cun plasma collià en moda inductiva. Lieus, nua che la surtratga antropogena da las concentraziuns d`elements era enconuschenta (funtaunas da puncts), èn vegnids exclus ordavant. Tar ils resultats da l`Atlas da terren geochemic sa tracti d`ina situaziun mumentana da las concentraziuns d`elements en las stresas superiuras da la Svizra (perioda da las emprovas: 2011-2015). Las chartas interpoladas servan a visualisar meglier regiuns cun concentraziuns augmentadas resp. bassas. I na pon dentant vegnir deducidas naginas infurmaziuns per singulas parcellas u conclusiuns definitivas a la geologia, a la biodisponibilitad, a la repartiziun procentuala da las funtaunas geogenas ed antropogenas u a la concentraziun dal terren. Citat: J. E. Reusser, M. B. Siegenthaler, L. H. E. Winkel, D. Wächter, R. Kretzschmar, R. G. Meuli: Geochemischer Bodenatlas der Schweiz. Agroscope, Zürich, 2023.</Abstract>
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        <Abstract>Concentraziuns d`elements interpoladas (mg/kg terra fina) en las stresas superiuras (0-20 cm) da la Svizra. Per las interpolaziuns d`Ordinary Kriging (1 km x 1 km) èn vegnidas resguardadas las datas da mesiraziuns da tut en tut 1201 lieus dal Monitoring da la biodiversitad en Svizra (MBD), da l`Observatori naziunal dal terren (NABO) e da l`Atlas da terren geochemic europeic (GEMAS). Las concentraziuns d`elements èn vegnidas analisadas en cumpariziuns d`aua roiala (HNO3:HCl:H2O) da provas da terren setgentadas (40 °C), crivladas (&lt; 2 mm) e silsuenter mieutas, quai cun agid da la spectrometria da massa cun plasma collià en moda inductiva. Lieus, nua che la surtratga antropogena da las concentraziuns d`elements era enconuschenta (funtaunas da puncts), èn vegnids exclus ordavant. Tar ils resultats da l`Atlas da terren geochemic sa tracti d`ina situaziun mumentana da las concentraziuns d`elements en las stresas superiuras da la Svizra (perioda da las emprovas: 2011-2015). Las chartas interpoladas servan a visualisar meglier regiuns cun concentraziuns augmentadas resp. bassas. I na pon dentant vegnir deducidas naginas infurmaziuns per singulas parcellas u conclusiuns definitivas a la geologia, a la biodisponibilitad, a la repartiziun procentuala da las funtaunas geogenas ed antropogenas u a la concentraziun dal terren. Citat: J. E. Reusser, M. B. Siegenthaler, L. H. E. Winkel, D. Wächter, R. Kretzschmar, R. G. Meuli: Geochemischer Bodenatlas der Schweiz. Agroscope, Zürich, 2023.</Abstract>
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        <Abstract>En il rom da l`Observaziun naziunala da la qualitad da las auas da surfatscha (NAWA) vegn registrada cuminaivlamain da la Confederaziun e dals chantuns la qualitad da l`aua a var 100 lieus da mesiraziun. La valitaziun dal stadi biologic da las auas sin basa d`examinaziuns da peschs vegn fatga tenor il modul &#39;peschs&#39; dal concept da moduls e da livels (www.modul-stufen-konzept.ch). En quasi tut ils auals e flums vivan peschs. Pervia da lur pretensiuns cumplexas e marcantas envers ils spazis da viver èn els buns indicaturs per il stadi morfologic ed idrologic da las auas. La mobilitad ed il cumportament da viadi da bleras spezias da peschs permettan er da trair conclusiuns davart la permeabilitad e la colliaziun da las auas.</Abstract>
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        <Abstract>En il rom da l`Observaziun naziunala da la qualitad da las auas da surfatscha (NAWA) vegn registrada cuminaivlamain da la Confederaziun e dals chantuns la qualitad da l`aua a var 100 lieus da mesiraziun. La valitaziun dal stadi biologic da las auas sin basa d`examinaziuns dals macrofits vegn fatga tenor la metoda dal chantun Turitg (www.gewaesserqualitaet.zh.ch/fg_methoden). Pervia da lur dependenza dal lieu e da lur lunga vita mussan plantas da l`aua (macrofits) sco plantas da scherm, mistgels ed algas visiblas ad egl las cundiziuns ch`èn avant maun en l`aua. Ellas inditgeschan la totalitad da las cundiziuns da l`ambient, spezialmain las relaziuns idraulicas-structuralas en l`aua.</Abstract>
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        <Abstract>En il rom da l`Observaziun naziunala da la qualitad da las auas da surfatscha (NAWA) vegn registrada cuminaivlamain da la Confederaziun e dals chantuns la qualitad da l`aua a var 100 lieus da mesiraziun. La valitaziun dal stadi biologic da las auas sin basa d`examinaziuns da macrozoobentos vegn fatga tenor il modul &#39;macrozoobentos&#39; dal concept da moduls e da livels (www.modul-stufen-konzept.ch). I vegn fatg quint ch`in disturbi antropogen da las auas currentas chaschunia per regla in regress da la diversitad biologica, da la quala èn pertutgads spezialmain tscherts insects. Sco macrozoobentos vegnan designads ils micro-organissems invertebrats che vivan giu al fund da l`aua. Ils micro-organissems invertebrats cun lur ciclus da vita, che ha lieu per ina part essenziala en l`aua, èn adattads sco bioindicaturs, perquai ch`els integreschan il stadi da l`aua durant lur entira existenza en l`aua e perquai ch`ins enconuscha savens bain lur pretensiuns a la qualitad da l`aua ed al spazi da viver.</Abstract>
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        <Abstract>En il rom da l`Observaziun naziunala da la qualitad da las auas da surfatscha (NAWA) vegn registrada cuminaivlamain da la Confederaziun e dals chantuns la qualitad da l`aua a var 100 lieus da mesiraziun. Il giudicament dal stadi chemic da las auas sin basa da la concentraziun d`ammonium vegn fatg tenor la metoda &#39;Retschertgas chemicas-fisicalas, substanzas nutritivas&#39; dal concept da moduls e da livels (www.modul-stufen-konzept.ch). Nitrogen è ina substanza nutritiva essenziala per organissems da l`aua. La part la pli gronda da nitrogen anorganic è avant maun en las auas en furma da nitrat. Sche l`oxigen manca, pon sa sviluppar or dal nitrat cumposiziuns da nitrogen reducidas, p.ex. ammonium (NH4+). Sche la valur pH crescha en l`aua, crescha er la part da l`ammonium ch`è avant maun sco amoniac (NH3) ch`è toxic per ils peschs. La concentraziun d`ammonium mussa la contaminaziun d`ina aua cun substanzas nuschaivlas che derivan da las auas persas communalas e d`imports che vegnan chaschunads da schlavaments e d`erosiuns da territoris duvrads da l`agricultura. Las pretensiuns numericas en l`Ordinaziun davart la protecziun da las auas per l`ammonium importa 0,2 mg/L N per ina temperatura da l`aua sur 10°C e 0,4 mg/L N per ina temperatura da l`aua sut 10°C.</Abstract>
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        <Abstract>En il rom da l`Observaziun naziunala da la qualitad da las auas da surfatscha (NAWA) vegn registrada cuminaivlamain da la Confederaziun e dals chantuns la qualitad da l`aua a var 100 lieus da mesiraziun. En l`unitad da datas qua avant maun è vegnida duvrada la pretensiun numerica da 4 mg/L per il giudicament. Il carbon organic dissolvì (DOC = dissolved organic carbon) po esser in indicatur per la contaminaziun d`ina aua tras la civilisaziun. Il DOC sa cumpona d`ina part ch`è avant maun da natira e d`ina part che deriva da la civilisaziun. L`Ordinaziun davart la protecziun da las auas prescriva sco pretensiun numerica in sectur per il DOC dad 1 fin 4 mg/L C. Il giudicament dal stadi chemic da las auas sin basa da la concentraziun da DOC vegn fatg tenor la metoda &#39;Retschertgas chemicas-fisicalas, substanzas nutritivas&#39; dal concept da moduls e da livels (www.modul-stufen-konzept.ch).</Abstract>
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        <Abstract>En il rom da l`Observaziun naziunala da la qualitad da las auas da surfatscha (NAWA) vegn registrada cuminaivlamain da la Confederaziun e dals chantuns la qualitad da l`aua a var 100 lieus da mesiraziun. Il giudicament dal stadi chemic da las auas sin basa da la concentraziun da nitrat vegn fatg tenor la metoda &#39;Retschertgas chemicas-fisicalas, substanzas nutritivas&#39; dal concept da moduls e da livels (www.modul-stufen-konzept.ch). Nitrogen è ina substanza nutritiva essenziala per organissems da l`aua e vegn absorbà da las plantas oravant tut en furma da nitrat (NO3-). La part la pli gronda da nitrogen anorganic è avant maun en las auas en furma da nitrat. Che algas e plantas na creschissan betg pli pervia d`ina concentraziun da nitrat memia pitschna è l`excepziun per auas currentas da la Svizra. Effects negativs sin las cuminanzas da vita en auas da surfatscha chaschunads da concentraziuns da nitrat sut 10 mg/L N na vegnan betg observads. Concentraziuns da nitrat sur 1,5 mg/L N derivan savens d`imports che vegnan chaschunads da schlavaments e d`erosiuns da territoris duvrads da l`agricultura ed er da l`inducziun d`auas persas communalas. La pretensiun numerica en l`Ordinaziun davart la protecziun da las auas per nitrat en las auas che vegnan duvradas sco aua da baiver, importa 5,6 mg/L N.</Abstract>
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        <Abstract>En il rom da l`Observaziun naziunala da la qualitad da las auas da surfatscha (NAWA) vegn registrada cuminaivlamain da la Confederaziun e dals chantuns la qualitad da l`aua a var 100 lieus da mesiraziun. Il giudicament dal stadi chemic da las auas sin basa da la concentraziun da nitrit vegn fatg tenor la metoda &#39;Retschertgas chemicas-fisicalas, substanzas nutritivas&#39; dal concept da moduls e da livels (www.modul-stufen-konzept.ch). Nitrogen è ina substanza nutritiva essenziala per organissems da l`aua. La part la pli gronda da nitrogen anorganic è avant maun en las auas en furma da nitrat. Sche l`oxigen manca, pon sa sviluppar or dal nitrat cumposiziuns da nitrogen reducidas, p.ex. nitrit (NO2-). Nitrit è in tissi fitg ferm per ils peschs, spezialmain per salmonids.</Abstract>
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        <Abstract>En il rom da l`Observaziun naziunala da la qualitad da las auas da surfatscha (NAWA) vegn registrada cuminaivlamain da la Confederaziun e dals chantuns la qualitad da l`aua a var 100 lieus da mesiraziun. Il giudicament dal stadi chemic da las auas sin basa da la concentraziun da fosfat vegn fatg tenor la metoda &#39;Retschertgas chemicas-fisicalas, substanzas nutritivas&#39; dal concept da moduls e da livels (www.modul-stufen-konzept.ch). Ortofosfat (PO43-) è la cumponenta da fosfor ch`è fisiologicamain activa en moda directa per plantas ed è in indicatur per la contaminaziun antropogena d`ina aua tras substanzas nutritivas. Cuntrari a lais n`ha il fosfor en auas currentas normalmain betg in effect limitant per il creschament da las algas e da las plantas. Pia n`è ina concentraziun da fosfat pli gronda en in`aua currenta betg in privel d`eutrofisaziun per l`aua, ella na correspunda però betg al stadi natiral pervia da l`immissiun antropogena.</Abstract>
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        <Abstract>En il rom da l`Observaziun naziunala da la qualitad da las auas da surfatscha (NAWA) vegn registrada cuminaivlamain da la Confederaziun e dals chantuns la qualitad da l`aua a var 100 lieus da mesiraziun. Il giudicament dal stadi chemic da las auas sin basa da la concentraziun totala da fosfor vegn fatg tenor la metoda &#39;Retschertgas chemicas-fisicalas, substanzas nutritivas&#39; dal concept da moduls e da livels (www.modul-stufen-konzept.ch). Fosfor è ina substanza nutritiva essenziala per organissems da l`aua. Il fosfor arriva en las auas en moda diffusa nà da l`agricultura, mintgatant sur inducziuns d`aua persa e sur sursculs en cas da plievgias ubain tras l`erosiun da crappa che cuntegna fosfor. Cuntrari a lais n`ha il fosfor en auas currentas normalmain betg in effect limitant per il creschament da las algas e da las plantas. Perquai ch`ils apports da funtaunas natiralas èn per regla minims, è il total da fosfor pia primarmain in indicatur per contaminaziuns antropogenas.</Abstract>
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        <Abstract>Immissiuns da fosfor en las auas èn ina contaminaziun nungiavischada. Tut en tut arrivan mintga onn var 3400 t fosfor total (fosfor dissolvì e fosfor particular) da funtaunas diffusas en las auas svizras. Grondas immissiuns derivan oravant tut da l`erosiun natirala en las Alps en furma da fosfor particular. Quel n`ha strusch in effect eutrof. Las calculaziuns da las immissiuns da fosfor tras erosiun natirala èn ultra da quai fitg intschertas. Mo 31 % da las immissiuns diffusas da fosfor total derivan da la surfatscha agricula.&lt;/p&gt;&lt;p&gt; Las immissiuns da fosfor total en las auas èn vegnidas calculadas cun il model da flussiun da substanzas MODIFFUS per tut las funtaunas d`immissiuns diffusas (ers, prads permanents, guauds, glatschers, surfatschas verdas dals abitadis e.u.v.) e per tut las vias d`immissiuns diffusas (erosiun dal terren, schlavament, drenascha, deposiziun atmosferica e.u.v.). La charta mussa las perditas cumuladas per categoria d`utilisaziun dal terren en il raster da hectaras sin basa da la statistica d`areals 2013/18. Per la calculaziun èn vegnidas duvradas cundiziuns climaticas mesaunas, cun l`onn da referenza 2020. &lt;/p&gt;&lt;p&gt; Questas valurs modelladas n`èn betg cumparegliablas cun valurs mesiradas en las auas, perquai ch`ellas na resguardan betg ils process da transfurmaziun e da sedimentaziun, ni en la cuntrada ni en las auas sezzas. Ils resultats pon vegnir interpretads per unitads idrologicas u administrativas a partir da 50 km2, dentant betg per singuls pixels.</Abstract>
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        <Abstract>Immissiuns da fosfor en las auas èn ina contaminaziun nungiavischada. Immissiuns pli grondas da fosfor dissolvì han chaschunà ils ultims decennis ina surladada dals lais da la Bassa. Tut en tut arrivan ca. 740 t fosfor dissolvì per onn da funtaunas diffusas en las auas svizras. Grondas immissiuns derivan cunzunt da pastgiras utilisadas en moda intensiva sin spundas. &lt;/p&gt;&lt;p&gt;Las immissiuns da fosfor en las auas èn vegnidas calculadas cun il model da flussiun da substanzas MODIFFUS per tut las funtaunas d`immissiuns diffusas (ers, prads permanents, guauds, glatschers, surfatschas verdas dals abitadis e.u.v.) e per lur vias d`apport (schlavament, drenascha, deposiziun atmosferica e.u.v.). La charta mussa las perditas cumuladas per categoria d`utilisaziun dal terren en il raster d`hectaras sin basa da la statistica d`areals 2013/18. Per la calculaziun èn vegnidas duvradas cundiziuns climaticas mesaunas, cun l`onn da referenza 2020. &lt;/p&gt;&lt;p&gt; Questas valurs modelladas n`èn betg cumparegliablas cun valurs mesiradas en las auas, perquai ch`ellas na resguardan betg ils process da transfurmaziun e da sedimentaziun en la cuntrada ed er betg en las auas sezzas. Ils resultats pon vegnir interpretads per unitads idrologicas u administrativas a partir d`in grondezza da 50 km², betg dentant per singuls pixels.</Abstract>
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        <Abstract>Immissiuns da nitrogen en las auas èn ina contaminaziun nungiavischada. En il rom da la Convenziun davart la protecziun da l`ambient maritim da l`Atlantic dal Nordost (OSPAR) è la Svizra s`obligada da reducir per 50% il volumen da nitrogen che sorta da la Svizra sur il Rain, cumpareglià cun l`onn 1985. Questa finamira n`è betg anc cuntanschida. Tut en tut arrivan ca. 48`000 t nitrogen per onn da funtaunas diffusas en las auas svizras. Grondas immissiuns derivan da surfatschas d`ers, en spezial da surfatschas drenadas. &lt;/p&gt;&lt;p&gt;Las immissiuns da nitrogen en las auas èn vegnidas calculadas cun il model da flussiun da substanzas MODIFFUS per tut las funtaunas d`immissiuns diffusas (ers, prads permanents, guauds, glatschers, surfatschas verdas dals abitadis e.u.v.) e per lur vias d`apport (erosiun dal terren, schlavament, drenascha, deposiziun atmosferica e.u.v.). La charta mussa las perditas cumuladas per categoria d`utilisaziun dal terren en il raster d`hectaras sin basa da la statistica d`areals 2013/18. Per la calculaziun èn vegnidas duvradas cundiziuns climaticas mesaunas, cun l`onn da referenza 2020. &lt;/p&gt;&lt;p&gt; Questas valurs modelladas n`èn betg cumparegliablas cun valurs mesiradas en las auas, perquai ch`ellas na resguardan betg ils process da transfurmaziun e da sedimentaziun en la cuntrada ed er betg en las auas sezzas. Ils resultats pon vegnir interpretads per unitads idrologicas u administrativas a partir d`in grondezza da 50 km2, betg dentant per singuls pixels</Abstract>
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        <Abstract>Tgi che vul prelevar aua d`in curs d`aua cun deflussiun permanenta (durant l`entir onn), saja quai per producir electricitad, per sauar u per sfradentar, dovra ina permissiun. Questa permissiun vegn dada mo, sch`ina quantitad d`aua adequata resta en il letg dal flum u da l`aual. Applitgadas vegnan questas prescripziuns d`aua restanta tenor la Lescha davart la protecziun da las auas mo en cas da novas prelevaziuns d`aua sco er en cas da prelevaziuns existentas, sche la concessiun scada e sto perquai vegnir renovada. La quantitad da deflussiun Q347 è ina da las basas per fixar las quantitads minimalas d`aua restanta. Per determinar la Q347 dovri mesiraziuns u proceduras adequatas da stimaziun. La charta &#39;Determinaziun da la quantitad da deflussiun Q347&#39; resumescha valurs da mesiraziun e da model. Las valurs da model èn stimaziuns approximativas che pon vegnir precisadas cun metodas pli raffinadas. Ina valur da stimaziun obtegnida en questa moda sto tuttina vegnir controllada en general a maun da mesiraziuns realas da curta durada.</Abstract>
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        <Abstract>L`aua sutterrana sa furma tras l`infiltraziun da l`aua da precipitaziuns sco er da l`aua da flums. Ils livels da l`aua sutterrana ed ils volumens d`aua da las funtaunas reageschan perquai - bain cun in pau retard - sin precipitaziuns e sin periodas da setgira. Il stadi ed il svilup dals livels da l`aua sutterrana e dals volumens d`aua da las funtaunas vegnan registrads en il rom dal modul QUANT da l`Observaziun naziunala da l`aua sutterrana NAQUA. La rait da mesiraziun dal modul QUANT cumpiglia ca. 100 posts da mesiraziun. Ella vegn manada dal UFAM en stretga collavuraziun cun ils posts chantunals spezialisads. Funtauna: Observaziun naziunala da l`aua sutterrana NAQUA, Uffizi federal d`ambient.</Abstract>
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        <Abstract>La charta mussa las deflussiuns actualas dals curs d`aua da la Svizra ed ils livels actuals da l`aua dals lais svizzers cumpareglià cun ils percentils mensils da las medias per ura da blers onns (indicaziun en percentils). Ils percentils vegnan calculads per mintga mais sin basa da las retschas da blers onns da las medias per ura. Per mintga mais vegnan cumpiladas separadamain las medias per ura davent dal cumenzament da las mesiraziuns fin oz. Il percentil definescha, tge part da las valurs ch`è pli gronda u pli pitschna ch`ina tscherta limita. Ina valur da deflussiun sin il percentil da 95% vul dir che 95% da las deflussiuns mesiradas durant il mais respectiv sa chattan sut questa sava (mo 5% èn sura).</Abstract>
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        <Abstract>Die Hochwasserwarnkarte zeigt die aktuelle Hochwassergefahr (Stufe 1 bis 5) für alle Fliessgewässer und Seen von gesamtschweizerischem Interesse sowie für die Regionen in Bezug auf kleine und mittlere Fliessgewässer.Die Fliessgewässer von gesamtschweizerischem Interesse sind in einzelne Flussabschnitte unterteilt. Zu jedem einzelnen Flussabschnitt ist eine Abflussmessstation definiert. Die Vorhersage beruht auf einem hydrologischen Modell und verschiedenen Wettermodellen. Abhängig von der Einschätzung und Interpretation der verschiedenen Modelle durch die Prognostikerinnen und Prognostiker werden die einzelnen Flussabschnitte und Seen entsprechend der Gefahrenstufe farblich gekennzeichnet. Bei Bedarf fordern die Prognostikerinnen und Prognostiker des BAFU bei MeteoSchweiz und/oder dem WSL-Institut für Schnee- und Lawinenforschung SLF genauere Auskünfte über die Wetterentwicklung und den Zustand der Schneedecke an. Das BAFU warnt und informiert auch dann, wenn lokal mit einem starken Anstieg der Abflüsse an kleinen und mittelgrossen Fliessgewässern zu rechnen ist. In solchen Fällen - insbesondere bei Gewittern mit Starkregen - kann nicht präzise vorausgesagt werden, welche Gewässer betroffen sein werden. Deshalb werden die voraussichtlich betroffenen Regionen auf der Hochwasserwarnkarte gekennzeichnet. Für kleine und mittelgrosse Fliessgewässer werden wegen den grösseren Unsicherheiten nur drei Gefahrenstufen unterschieden: keine oder geringe Gefahr (grün), mässige Hochwassergefahr (gelb) und grosse Hochwassergefahr (rot).</Abstract>
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        <Abstract>L`effectiv d`edifizis svizzers è responsabel per circa in quart da las emissiuns da CO₂. Per cuntanscher las finamiras dal clima èn las reducziuns en quest sectur centralas.&lt;/p&gt;&lt;p&gt; Cun la charta `Emissiuns da CO₂ Edifizis (SIA 380/1)` pon ins stimar, quant CO₂ che mintga edifizi d`abitar emetta. Questas emissiuns da CO₂ vegnan calculadas per il basegn d`energia termica e d`aua chauda sut cundiziuns da referenza. Per la calculaziun vegnan integradas las datas publicas d`input dal register federal dals edifizis e da las abitaziuns REA da l`Uffizi federal da statistica. Questas datas n`èn betg actualas per mintga lieu ed ellas na cuntegnan naginas infurmaziuns suffizientas davart las sanaziuns d`edifizis. Cun il calculatur interactiv da CO₂ èsi pussaivel da simular, co che la valur da CO₂ sa mida, sch`er sanaziuns energeticas vegnan resguardadas u sch`i vegn midà il purtader d`energia. Las datas endatadas na vegnan betg arcunadas. Quest tool pudais Vus utilisar per mintga edifizi sut `Infurmaziun da l`object`.&lt;/p&gt;&lt;p&gt; Las indicaziuns ston vegnir chapidas sco stimaziun approximativa e na represchentan naginas indicaziuns uffizialas u liantas.&lt;/p&gt;&lt;p&gt; La visualisaziun dal CO₂ cun il calculatur da CO₂ procura per transparenza e mussa, ch`igl è spezialmain impurtant d`actualisar cuntinuadamain las datas dal REA. Persunas che possedan edifizis pon sezzas gidar da mantegnair actualas las datas dal REA ch`èn relevantas per il clima e l`energia. En in link sut `Infurmaziun da l`object` chattan ins tar mintga edifizi la descripziun, co ch`ins po annunziar indicaziuns ch`èn eventualmain antiquadas.&lt;/p&gt;&lt;p&gt; Ulteriuras infurmaziuns chattais Vus sut https://www.bafu.admin.ch/de/co2-rechner-gebaeude.</Abstract>
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        <Abstract>Infurmaziuns davart l`autezza da la vegetaziun vegnan retschertgadas cun metodas da l`exploraziun a distanza cun sensurs activs e passivs. In sensur activ è LiDAR. In sensur passiv è in sensur optic, per exempel ina camera per fotografias ord l`aria. LiDAR vegn duvrà en Svizra sin plaun regiunal, chantunal e naziunal. Fotografias da stereo or da l`aria vegnan registradas regularmain sin plaun naziunal en in turnus da 3 onns. Da questas datas da basa da swisstopo planisablas vegnan fatgs regularmain unitads da datas en 3D, models digitals da la surfatscha (MDS), cun auta resoluziun en il rom da l`Inventari forestal naziunal (IFN). Da la differenza dal MDS e dal model digital dal terren da swisstopo (swissAlti3D) vegn calculà in model digital da la surfatscha normalisà (MDSn). Edifizis vegnan eliminads cun ina cumbinaziun da las surfatschas da basa dal model topografic da la cuntrada (MTC) da swisstopo e da las infurmaziuns spectralas da las fotografias da stereo ord l`aria. Il resultat final è in model d`autezza da la vegetaziun (MAV) da la Svizra.</Abstract>
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        <Abstract>Per la rait d`auas da la Svizra èn vegnidas modelladas las deflussiuns (m³/s) mensilas ed annualas natiralas mesaunas e vegnids eruids ils tips d`urden da deflussiun appartegnents. Cun `MQ-GWN-CH` è avant maun per tut las auas da grondezza mesauna ina basa da datas davart las deflussiuns mesaunas. Naginas valurs da deflussiun n`existan per auas cun intschess &lt; 3 km² (limita da las basas idrologicas duvradas per la modellaziun) e &gt;= 500 km² (perquai ch`i vegn presumà ch`i existian per quest intent per regla staziuns da mesiraziun da la deflussiun adequatas). En general vala che las mesiraziuns da las staziuns idrometricas furman ina meglra basa da datas.</Abstract>
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        <Abstract>La charta mussa las midadas procentualas calculadas en ils scenaris idrologics Hydro-CH2018 da las deflussiuns da stad vers la fin dal tschientaner (2070 - 2099) en cumparegliaziun cun la perioda da referenza (1981 - 2010) per in scenari senza protecziun dal clima (RCP8.5). Preschentà vegn mintgamai il median da l`entira dimensiun da tut las simulaziuns. Durant la stad mussan ils scenaris idrologics ina reducziun media da la deflussiun da 30 - 50 % senza protecziun dal clima fin la fin dal tschientaner. Responsablas per questa reducziun èn las precipitaziuns da stad pli pitschnas, ina svapuraziun pli gronda e la reducziun da l`aua da glatschers e da l`aua da naiv luada. En il project Hydro-CH2018 ch`è in accent tematic dal National Centre for Climate Services (NCCS, www.nccs.admin.ch) e che vegn manà dal UFAM, èn vegnids applitgads - tut tenor la dumonda - differents models idrologics spezialisads. Pervia da quai èsi pussaivel, ch`i èn avant maun plirs resultats per tschertas staziuns, che divergeschan levamain in da l`auter, p.ex. la Thur ad Andelfingen (detagls en quest connex pon vegnir consultads en il rapport da sintesa `Consequenzas da la midada dal clima sin las auas svizras`). Cun cliccar sin il link en las infurmaziuns da l`object arrivais Vus a l`Atlas idrologic da la Svizra, nua che Vus chattais tut ils resultats per tut las staziuns, per tut ils scenaris climatics e per tut las periodas incl. il sectur da malsegirezza.</Abstract>
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        <Abstract>La charta mussa tut ils lieus enconuschents en Svizra, nua ch`ins ha chattà mistgels periclitads e protegids. Resguardads èn ils chats da spezias da la Glista cotschna da las categorias CR (en privel da svanir), EN (fitg periclitadas), VU (vulnerablas) e RE (svanidas en Svizra) sco er ils chats da tut las spezias ch`èn protegidas sin plaun naziunal u chantunal tras l`Ordinaziun davart la protecziun da la natira e da la patria (OPNP). Sin la charta inditgescha in punct in lieu da chat exact (cun ina toleranza da 10 m resp. da 100 m). Sche mo il kilometer quadrat dal lieu da chat è enconuschent, è il punct inditgà giusum a sanestra sin il tagl da las coordinatas.</Abstract>
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      <Abstract>Nitrat è ina substanza nutritiva essenziala per las plantas. En l`aua sutterrana arriva il nitrat principalmain tras ladims da bains purils u ladims minerals danvanz. Tenor l`Ordinaziun davart la protecziun da las auas OPAuas dastga l`aua sutterrana avair ina concentraziun da nitrat da maximalmain 25 mg/l. La concentraziun da nitrat en l`aua sutterrana da la Svizra vegn registrada sin plaun naziunal en il rom da l`Observaziun naziunala da l`aua sutterrana NAQUA. La rait da mesiraziun da l`Observaziun naziunala da l`aua sutterrana cumpiglia passa 500 posts da mesiraziun e vegn manada dal UFAM en stretga collavuraziun cun ils chantuns. Funtauna: Observaziun naziunala da l`aua sutterrana NAQUA, Uffizi federal d`ambient.</Abstract>
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        <Abstract>Il set &#39;Plantas exoticas invasivas&#39; cuntegna las chartas da la derasaziun potenziala da 56 spezias exoticas invasivas che creschan en Svizra sco er da spezias exoticas invasivas che creschan en pajais vischins e che han il potenzial da sa derasar en Svizra. Las chartas èn il resultat d`ina modellaziun da l`Universitad da Losanna che duai prognostitgar la derasaziun da plantas invasivas che figureschan sin la Glista naira resp. sin la &#39;Watch list&#39;. Il model sa basa sin las datas disponiblas dal GBIF (Global Biodiversity Information Facility), cumbinà cun datas climaticas da Worldclim (resoluziun dad 1 km), sco er sin las datas disponiblas dad InfoFlora, cumbinà cun las datas climaticas dal WSL (resoluziun da 100 m). Las chartas cun ina resoluziun da 100 m cuntegnan ulteriuras variablas sco l`utilisaziun dal terren e la geologia.</Abstract>
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        <Abstract>Il set &#39;Plantas exoticas invasivas&#39; cuntegna las chartas da la derasaziun potenziala da 56 spezias exoticas invasivas che creschan en Svizra sco er da spezias exoticas invasivas che creschan en pajais vischins e che han il potenzial da sa derasar en Svizra. Las chartas èn il resultat d`ina modellaziun da l`Universitad da Losanna che duai prognostitgar la derasaziun da plantas invasivas che figureschan sin la Glista naira resp. sin la &#39;Watch list&#39;. Il model sa basa sin las datas disponiblas dal GBIF (Global Biodiversity Information Facility), cumbinà cun datas climaticas da Worldclim (resoluziun dad 1 km), sco er sin las datas disponiblas dad InfoFlora, cumbinà cun las datas climaticas dal WSL (resoluziun da 100 m). Las chartas cun ina resoluziun da 100 m cuntegnan ulteriuras variablas sco l`utilisaziun dal terren e la geologia.</Abstract>
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        <Abstract>Il set &#39;Plantas exoticas invasivas&#39; cuntegna las chartas da la derasaziun potenziala da 56 spezias exoticas invasivas che creschan en Svizra sco er da spezias exoticas invasivas che creschan en pajais vischins e che han il potenzial da sa derasar en Svizra. Las chartas èn il resultat d`ina modellaziun da l`Universitad da Losanna che duai prognostitgar la derasaziun da plantas invasivas che figureschan sin la Glista naira resp. sin la &#39;Watch list&#39;. Il model sa basa sin las datas disponiblas dal GBIF (Global Biodiversity Information Facility), cumbinà cun datas climaticas da Worldclim (resoluziun dad 1 km), sco er sin las datas disponiblas dad InfoFlora, cumbinà cun las datas climaticas dal WSL (resoluziun da 100 m). Las chartas cun ina resoluziun da 100 m cuntegnan ulteriuras variablas sco l`utilisaziun dal terren e la geologia.</Abstract>
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        <Abstract>Il set &#39;Plantas exoticas invasivas&#39; cuntegna las chartas da la derasaziun potenziala da 56 spezias exoticas invasivas che creschan en Svizra sco er da spezias exoticas invasivas che creschan en pajais vischins e che han il potenzial da sa derasar en Svizra. Las chartas èn il resultat d`ina modellaziun da l`Universitad da Losanna che duai prognostitgar la derasaziun da plantas invasivas che figureschan sin la Glista naira resp. sin la &#39;Watch list&#39;. Il model sa basa sin las datas disponiblas dal GBIF (Global Biodiversity Information Facility), cumbinà cun datas climaticas da Worldclim (resoluziun dad 1 km), sco er sin las datas disponiblas dad InfoFlora, cumbinà cun las datas climaticas dal WSL (resoluziun da 100 m). Las chartas cun ina resoluziun da 100 m cuntegnan ulteriuras variablas sco l`utilisaziun dal terren e la geologia.</Abstract>
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        <Abstract>&lt;p&gt;Charta mensila dal potenzial erosiv da las precipitaziuns (factur R) da la Svizra en ina dissoluziun spaziala da 100 m. Las chartas mussan la variabilitad territoriala e stagiunala dal potenzial erosiv da las precipitaziuns en MJ mm ha⁻¹ h⁻¹ mais⁻¹. Las colurs blau cleras inditgan in effect erosiv pitschen, las colurs blau stgiras in effect erosiv grond da las precipitaziuns.&lt;/p&gt; &lt;p&gt;Ils facturs R mensils èn vegnids eruids sin basa da las mesiraziuns da las precipitaziuns dad 87 staziuns da mesiraziun automaticas cun intervals da mesiraziun da 10 minutas (media da la perioda da mesiraziun da 19,5 onns per staziun). Las staziuns resguardan tut las zonas agriculas da la Svizra. Per excluder l`influenza da la naiv vegnan ultra da quai registradas las temperaturas en pass d`ina ura en 71 staziuns u eruidas da la proxima staziun.&lt;/p&gt; &lt;p&gt;La cumparegliaziun da las 12 chartas mensilas dal factur R mussa ch`ils mais da stad (zercladur, fanadur ed avust) han - en quai che concerna il potenzial erosiv da las precipitaziuns - las valurs las pli autas durant l`onn. En spezial ils territoris da las Alps dal Sid (chantun Tessin), las zonas da muntogna da las Alps dal Nord e parts da la zona da la Svizra Bassa mussan auts facturs R per questa perioda. Tranter ils mais da zercladur e da settember vegn registrada ina quota da 62 % dal potenzial erosiv annual da las precipitaziuns en Svizra. L`identificaziun da regiuns e da periodas cun precipitaziuns cun in effect erosiv pli grond pussibilitescha ina protecziun sistematica cunter l`erosiun ed ina meglra chapientscha da las dinamicas da process d`erosiun durant in onn.&lt;/p&gt; La creaziun da las chartas mensilas dal potenzial erosiv da las precipitaziuns da la Svizra è descritta en detagl en &#39;Regionalization of monthly rainfall erosivity patterns in Switzerland&#39; da Schmidt et al. (Hydrology and Earth System Sciences: 20. 2016. p. 4359-4373).</Abstract>
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      <Abstract>Tenor l`Ordinaziun davart ils atterraments externs (OAEx; CS 748.132.3) cumpiglian ils territoris protegids parcs naziunals, palids autas e transiziunalas, reservats d`utschels da l`aua e d`utschels migrants, palids planivas, zonas umidas ed asils federals da selvaschina (art. 19 OAEx) sco er cuntradas da palì d`impurtanza naziunala (art. 32 lit. h OAEx). Atterraments externs (vul dir partir u atterrar sco er chargiar u stgargiar chaussas u persunas ordaifer las plazzas aviaticas) èn da princip scumandads per eromobils civils equipads en ils territoris protegids. Sin basa da las restricziuns e cundiziuns specificas per atterraments externs differenzieschan las publicaziuns d`aviatica tranter quatter categorias: 1. Asils da selvaschina; 2. Cuntradas da palì; 3. Zonas umidas; 4. Ulteriurs territoris protegids (palids autas e transiziunalas, palids planivas, reservats d`utschels da l`aua e d`utschels migrants, parcs naziunals). Mintga categoria da territoris protegids è dividida en dus nivels da generalisaziun: Sin las vistas da pitschna scala vegnan preschentads ils territoris protegids en ina furma generalisada ed indirectamain proporziunala tar la surfatscha cun ina zona da plimatsch tranter 1 ed 80 meters. Quai per avair ina meglra legibladad. En las vistas da gronda scala vegnan ils perimeters dals territoris protegids preschentads en lur extensiun giuridicamain valaivla. Atterraments externs en zonas umidas èn scumandads, cun resalva da l`art. 19 al. 3 e da l`art. 28 OAEx. Atterraments externs per la protecziun cunter privels da la natira sco er per la construcziun u il mantegniment d`edifizis e stabiliments d`in interess public èn admess. Er admess èn atterraments externs per incumbensa da las autoritads chantunalas cumpetentas sco er atterraments externs che questas autoritads han permess per la construcziun u il mantegniment d`edifizis e stabiliments.</Abstract>
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        <Abstract>Tenor l`Ordinaziun davart ils atterraments externs (OAEx; CS 748.132.3) cumpiglian ils territoris protegids parcs naziunals, palids autas e transiziunalas, reservats d`utschels da l`aua e d`utschels migrants, palids planivas, zonas umidas ed asils federals da selvaschina (art. 19 OAEx) sco er cuntradas da palì d`impurtanza naziunala (art. 32 lit. h OAEx). Atterraments externs (vul dir partir u atterrar sco er chargiar u stgargiar chaussas u persunas ordaifer las plazzas aviaticas) èn da princip scumandads per eromobils civils equipads en ils territoris protegids. Sin basa da las restricziuns e cundiziuns specificas per atterraments externs differenzieschan las publicaziuns d`aviatica tranter quatter categorias: 1. Asils da selvaschina; 2. Cuntradas da palì; 3. Zonas umidas; 4. Ulteriurs territoris protegids (palids autas e transiziunalas, palids planivas, reservats d`utschels da l`aua e d`utschels migrants, parcs naziunals). Mintga categoria da territoris protegids è dividida en dus nivels da generalisaziun: Sin las vistas da pitschna scala vegnan preschentads ils territoris protegids en ina furma generalisada ed indirectamain proporziunala tar la surfatscha cun ina zona da plimatsch tranter 1 ed 80 meters. Quai per avair ina meglra legibladad. En las vistas da gronda scala vegnan ils perimeters dals territoris protegids preschentads en lur extensiun giuridicamain valaivla. Atterraments externs en zonas umidas èn scumandads, cun resalva da l`art. 19 al. 3 e da l`art. 28 OAEx. Atterraments externs per la protecziun cunter privels da la natira sco er per la construcziun u il mantegniment d`edifizis e stabiliments d`in interess public èn admess. Er admess èn atterraments externs per incumbensa da las autoritads chantunalas cumpetentas sco er atterraments externs che questas autoritads han permess per la construcziun u il mantegniment d`edifizis e stabiliments.</Abstract>
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      <Abstract>Tenor l`Ordinaziun davart ils atterraments externs (OAEx; CS 748.132.3) cumpiglian ils territoris protegids parcs naziunals, palids autas e transiziunalas, reservats d`utschels da l`aua e d`utschels migrants, palids planivas, zonas umidas ed asils federals da selvaschina (art. 19 OAEx) sco er cuntradas da palì d`impurtanza naziunala (art. 32 lit. h OAEx). Atterraments externs (vul dir partir u atterrar sco er chargiar u stgargiar chaussas u persunas ordaifer las plazzas aviaticas) èn da princip scumandads per eromobils civils equipads en ils territoris protegids. Sin basa da las restricziuns e cundiziuns specificas per atterraments externs differenzieschan las publicaziuns d`aviatica tranter quatter categorias: 1. Asils da selvaschina; 2. Cuntradas da palì; 3. Zonas umidas; 4. Ulteriurs territoris protegids (palids autas e transiziunalas, palids planivas, reservats d`utschels da l`aua e d`utschels migrants, parcs naziunals). Mintga categoria da territoris protegids è dividida en dus nivels da generalisaziun: Sin las vistas da pitschna scala vegnan preschentads ils territoris protegids en ina furma generalisada ed indirectamain proporziunala tar la surfatscha cun ina zona da plimatsch tranter 1 ed 80 meters. Quai per avair ina meglra legibladad. En las vistas da gronda scala vegnan ils perimeters dals territoris protegids preschentads en lur extensiun giuridicamain valaivla. Atterraments externs en asils da selvaschina èn scumandads, cun resalva da l`art. 19 al. 3, da l`art. 28 e da l`art. 46 al. 4 OAEx. Atterraments externs per la protecziun cunter privels da la natira, per l`economia forestala e l`agricultura, per il provediment da chamonas accessiblas a la publicitad sco er per la construcziun u il mantegniment d`edifizis e stabiliments d`in interess public èn admess. Er admess èn atterraments externs e sgols ballantschads en il rom da sgols da scolaziun sco er atterraments per incumbensa da las autoritads chantunalas cumpetentas ed atterraments externs che questas autoritads han permess per la construcziun u il mantegniment d`edifizis e stabiliments d`in interess public. Per sgols per auters intents da lavur vala il scumonda mo dal 1. da november fin ils 31 da fanadur.</Abstract>
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        <Abstract>Tenor l`Ordinaziun davart ils atterraments externs (OAEx; CS 748.132.3) cumpiglian ils territoris protegids parcs naziunals, palids autas e transiziunalas, reservats d`utschels da l`aua e d`utschels migrants, palids planivas, zonas umidas ed asils federals da selvaschina (art. 19 OAEx) sco er cuntradas da palì d`impurtanza naziunala (art. 32 lit. h OAEx). Atterraments externs (vul dir partir u atterrar sco er chargiar u stgargiar chaussas u persunas ordaifer las plazzas aviaticas) èn da princip scumandads per eromobils civils equipads en ils territoris protegids. Sin basa da las restricziuns e cundiziuns specificas per atterraments externs differenzieschan las publicaziuns d`aviatica tranter quatter categorias: 1. Asils da selvaschina; 2. Cuntradas da palì; 3. Zonas umidas; 4. Ulteriurs territoris protegids (palids autas e transiziunalas, palids planivas, reservats d`utschels da l`aua e d`utschels migrants, parcs naziunals). Mintga categoria da territoris protegids è dividida en dus nivels da generalisaziun: Sin las vistas da pitschna scala vegnan preschentads ils territoris protegids en ina furma generalisada ed indirectamain proporziunala tar la surfatscha cun ina zona da plimatsch tranter 1 ed 80 meters. Quai per avair ina meglra legibladad. En las vistas da gronda scala vegnan ils perimeters dals territoris protegids preschentads en lur extensiun giuridicamain valaivla. Atterraments externs en asils da selvaschina èn scumandads, cun resalva da l`art. 19 al. 3, da l`art. 28 e da l`art. 46 al. 4 OAEx. Atterraments externs per la protecziun cunter privels da la natira, per l`economia forestala e l`agricultura, per il provediment da chamonas accessiblas a la publicitad sco er per la construcziun u il mantegniment d`edifizis e stabiliments d`in interess public èn admess. Er admess èn atterraments externs e sgols ballantschads en il rom da sgols da scolaziun sco er atterraments per incumbensa da las autoritads chantunalas cumpetentas ed atterraments externs che questas autoritads han permess per la construcziun u il mantegniment d`edifizis e stabiliments d`in interess public. Per sgols per auters intents da lavur vala il scumonda mo dal 1. da november fin ils 31 da fanadur.</Abstract>
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      <Abstract>Tenor l`Ordinaziun davart ils atterraments externs (OAEx; CS 748.132.3) cumpiglian ils territoris protegids parcs naziunals, palids autas e transiziunalas, reservats d`utschels da l`aua e d`utschels migrants, palids planivas, zonas umidas ed asils federals da selvaschina (art. 19 OAEx) sco er cuntradas da palì d`impurtanza naziunala (art. 32 lit. h OAEx). Atterraments externs (vul dir partir u atterrar sco er chargiar u stgargiar chaussas u persunas ordaifer las plazzas aviaticas) èn da princip scumandads per eromobils civils equipads en ils territoris protegids. Sin basa da las restricziuns e cundiziuns specificas per atterraments externs differenzieschan las publicaziuns d`aviatica tranter quatter categorias: 1. Asils da selvaschina; 2. Cuntradas da palì; 3. Zonas umidas; 4. Ulteriurs territoris protegids (palids autas e transiziunalas, palids planivas, reservats d`utschels da l`aua e d`utschels migrants, parcs naziunals). Mintga categoria da territoris protegids è dividida en dus nivels da generalisaziun: Sin las vistas da pitschna scala vegnan preschentads ils territoris protegids en ina furma generalisada ed indirectamain proporziunala tar la surfatscha cun ina zona da plimatsch tranter 1 ed 80 meters. Quai per avair ina meglra legibladad. En las vistas da gronda scala vegnan ils perimeters dals territoris protegids preschentads en lur extensiun giuridicamain valaivla. Atterraments externs en cuntradas da palì èn scumandads per sgols betg commerzials tenor l`art. 32 lit. h OAEx.</Abstract>
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        <Abstract>Tenor l`Ordinaziun davart ils atterraments externs (OAEx; CS 748.132.3) cumpiglian ils territoris protegids parcs naziunals, palids autas e transiziunalas, reservats d`utschels da l`aua e d`utschels migrants, palids planivas, zonas umidas ed asils federals da selvaschina (art. 19 OAEx) sco er cuntradas da palì d`impurtanza naziunala (art. 32 lit. h OAEx). Atterraments externs (vul dir partir u atterrar sco er chargiar u stgargiar chaussas u persunas ordaifer las plazzas aviaticas) èn da princip scumandads per eromobils civils equipads en ils territoris protegids. Sin basa da las restricziuns e cundiziuns specificas per atterraments externs differenzieschan las publicaziuns d`aviatica tranter quatter categorias: 1. Asils da selvaschina; 2. Cuntradas da palì; 3. Zonas umidas; 4. Ulteriurs territoris protegids (palids autas e transiziunalas, palids planivas, reservats d`utschels da l`aua e d`utschels migrants, parcs naziunals). Mintga categoria da territoris protegids è dividida en dus nivels da generalisaziun: Sin las vistas da pitschna scala vegnan preschentads ils territoris protegids en ina furma generalisada ed indirectamain proporziunala tar la surfatscha cun ina zona da plimatsch tranter 1 ed 80 meters. Quai per avair ina meglra legibladad. En las vistas da gronda scala vegnan ils perimeters dals territoris protegids preschentads en lur extensiun giuridicamain valaivla. Atterraments externs en cuntradas da palì èn scumandads per sgols betg commerzials tenor l`art. 32 lit. h OAEx.</Abstract>
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      <Abstract>Tenor l`Ordinaziun davart ils atterraments externs (OAEx; CS 748.132.3) cumpiglian ils territoris protegids parcs naziunals, palids autas e transiziunalas, reservats d`utschels da l`aua e d`utschels migrants, palids planivas, zonas umidas ed asils federals da selvaschina (art. 19 OAEx) sco er cuntradas da palì d`impurtanza naziunala (art. 32 lit. h OAEx). Atterraments externs (vul dir partir u atterrar sco er chargiar u stgargiar chaussas u persunas ordaifer las plazzas aviaticas) èn da princip scumandads per eromobils civils equipads en ils territoris protegids. Sin basa da las restricziuns e cundiziuns specificas per atterraments externs differenzieschan las publicaziuns d`aviatica tranter quatter categorias: 1. Asils da selvaschina; 2. Cuntradas da palì; 3. Zonas umidas; 4. Ulteriurs territoris protegids (palids autas e transiziunalas, palids planivas, reservats d`utschels da l`aua e d`utschels migrants, parcs naziunals). Mintga categoria da territoris protegids è dividida en dus nivels da generalisaziun: Sin las vistas da pitschna scala vegnan preschentads ils territoris protegids en ina furma generalisada ed indirectamain proporziunala tar la surfatscha cun ina zona da plimatsch tranter 1 ed 80 meters. Quai per avair ina meglra legibladad. En las vistas da gronda scala vegnan ils perimeters dals territoris protegids preschentads en lur extensiun giuridicamain valaivla. Atterraments externs en ils ulteriurs territoris protegids èn scumandads, cun resalva da l`art. 19 al. 3 e da l`art. 28 OAEx.</Abstract>
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        <Abstract>Tenor l`Ordinaziun davart ils atterraments externs (OAEx; CS 748.132.3) cumpiglian ils territoris protegids parcs naziunals, palids autas e transiziunalas, reservats d`utschels da l`aua e d`utschels migrants, palids planivas, zonas umidas ed asils federals da selvaschina (art. 19 OAEx) sco er cuntradas da palì d`impurtanza naziunala (art. 32 lit. h OAEx). Atterraments externs (vul dir partir u atterrar sco er chargiar u stgargiar chaussas u persunas ordaifer las plazzas aviaticas) èn da princip scumandads per eromobils civils equipads en ils territoris protegids. Sin basa da las restricziuns e cundiziuns specificas per atterraments externs differenzieschan las publicaziuns d`aviatica tranter quatter categorias: 1. Asils da selvaschina; 2. Cuntradas da palì; 3. Zonas umidas; 4. Ulteriurs territoris protegids (palids autas e transiziunalas, palids planivas, reservats d`utschels da l`aua e d`utschels migrants, parcs naziunals). Mintga categoria da territoris protegids è dividida en dus nivels da generalisaziun: Sin las vistas da pitschna scala vegnan preschentads ils territoris protegids en ina furma generalisada ed indirectamain proporziunala tar la surfatscha cun ina zona da plimatsch tranter 1 ed 80 meters. Quai per avair ina meglra legibladad. En las vistas da gronda scala vegnan ils perimeters dals territoris protegids preschentads en lur extensiun giuridicamain valaivla. Atterraments externs en ils ulteriurs territoris protegids èn scumandads, cun resalva da l`art. 19 al. 3 e da l`art. 28 OAEx.</Abstract>
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        <Abstract>Ils territoris protegids tenor la charta militara d`obstachels da l`aviatica cumpiglian il Parc naziunal, palids autas, tschertas zonas umidas e palids planivas, reservats d`utschels da l`aua e d`utschels migrants sco er asils federals da selvaschina. Tar ils reservats d`utschels da l`aua e d`utschels migrants èn vegnids adattads ils perimeters d`intgins objects cun in`utilisaziun existenta. Tar las palids e tar las zonas umidas sper ils lais e per lung da las rivas dals flums han ils perimeters plinavant survegnì ina zona da plimatsch da 100 meters.</Abstract>
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        <Abstract>La Lescha federala davart la protecziun da la natira e da la patria (CS 451) definescha, suenter la revisiun dal 1. da december 2007, trais categorias da parcs d`impurtanza naziunala: parcs naziunals, parcs natirals regiunals e parcs natirals d`aventura. Tut tenor il stadi dal project pon las regiuns pertutgadas dumandar il label &#39;Candidatura&#39; per stabilir in parc u il label &#39;Parc&#39; (sco marca protegida) per manar il parc. Parcs d`impurtanza naziunala gidan a proteger ed ad augmentar la valur da spazis da viver natirals extraordinaris. A medem temp sustegnan ils parcs il svilup economic d`ina regiun. L`unitad da datas &#39;Parcs&#39; cuntegna supplementarmain ils projects da parcs ch`èn annunziads tar il UFAM sco er il territori da protecziun &#39;Parc naziunal svizzer&#39; ch`è protegì tenor la Lescha federala dals 19 da december 1980 davart il Parc naziunal (CS 454).</Abstract>
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        <Abstract>Sbuvadas vegnan giu sin spundas libras, independentamain d`in curs d`aua. Sbuvadas èn ina maschaida da crappa lucca (per il solit mo terren e vegetaziun) e da blera aua. Ellas sa distatgan da la surfatscha d`ina spunda e van a val cun gronda sveltezza. Tras quai ch`il process cuntegna relativamain blera aua, ha el ina gronda sveltezza (1 - 10 m/s) ed ina forza destructiva correspundenta. La surfatscha pertutgada dal transport da material è uschia savens 10 fin 100 giadas pli gronda che la surfatscha da distatga, ch`è savens fitg pitschna. Quest layer mussa ina charta d`infurmaziun da privels cun las surfatschas potenzialas da sbuvadas sin basa da modellaziuns dal process &#39;sbuvadas&#39; tenor il project SilvaProtect-CH.</Abstract>
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        <Abstract>Bovas èn ina maschaida d`aua e d`ina gronda quota da substanzas solidas (ca. 30% fin 60%) che van a val cun pitschna fin gronda sveltezza. Bovas vegnan savens giu en pliras giadas, e quai en torrents sco er da gondas stippas. Per las zonas d`abitadi cuntegnan ellas in grond potenzial da privel. Quest layer mussa ina charta d`infurmaziun da privels cun las surfatschas potenzialas da bovas sin basa da modellaziuns dal process &#39;bovas&#39; tenor il project SilvaProtect-CH.</Abstract>
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        <Title>Crudadas (SilvaProtect-CH)</Title>
        <Abstract>Crudadas da crappa e da grippa èn caracterisadas da moviments da cupitgada isolads (crudar, siglir, rudlar) da singuls craps u grips che pon avair ina grondezza da plirs meters cubic. Ils craps e grips pon cuntanscher sveltezzas fin 30 m/s. Sin spundas cun pendenzas da main che 30° sa ferman ils craps e grips en general. Il guaud po reducir fermamain l`energia chinetica dals blocs. Quest layer mussa ina charta d`infurmaziun da privels cun las trajectorias potenzialas da crudada da crappa e da grippa sin basa da modellaziuns dal process &#39;crudada da crappa e grippa&#39; tenor il project SilvaProtect-CH.</Abstract>
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        <Abstract>Sedimentaziuns alluvialas èn substanzas solidas (glera e grava) che sa depositeschan tras aua che curra ordaifer ses letg, per il solit en il sectur da cugns alluvials da torrents. Quest layer mussa ina charta d`infurmaziun da privels cun las surfatschas potenzialas da sedimentaziuns alluvialas sin basa da modellaziuns dal process &#39;sedimentaziuns alluvialas&#39; tenor il project SilvaProtect-CH.</Abstract>
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        <Abstract>La sesida plenara da la Cumissiun internaziunala per la protecziun dal Rain (CIPR) aveva incaricà l`onn 1999 sia gruppa da lavur Ecologia da descriver la structura dal flum e da preschentar tala sin ina charta a la scala 1:100`000. La Directiva generala europeica davart l`aua, che fixescha finamiras da qualitad cumparegliablas per las auas da la UE, pretenda l`inventarisaziun e la valitaziun da caracteristicas ecomorfologicas dals curs d`aua.</Abstract>
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        <Abstract>La sesida plenara da la Cumissiun internaziunala per la protecziun dal Rain (CIPR) aveva incaricà l`onn 1999 sia gruppa da lavur Ecologia da descriver la structura dal flum e da preschentar tala sin ina charta a la scala 1:100`000. La Directiva generala europeica davart l`aua, che fixescha finamiras da qualitad cumparegliablas per las auas da la UE, pretenda l`inventarisaziun e la valitaziun da caracteristicas ecomorfologicas dals curs d`aua.</Abstract>
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        <Abstract>La sesida plenara da la Cumissiun internaziunala per la protecziun dal Rain (CIPR) aveva incaricà l`onn 1999 sia gruppa da lavur Ecologia da descriver la structura dal flum e da preschentar tala sin ina charta a la scala 1:100`000. La Directiva generala europeica davart l`aua, che fixescha finamiras da qualitad cumparegliablas per las auas da la UE, pretenda l`inventarisaziun e la valitaziun da caracteristicas ecomorfologicas dals curs d`aua.</Abstract>
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        <Abstract>Las chartas da la periclitaziun tras stemprads mussan ils bufs sco er lur pressiuns dinamicas inclusiv las intschertezzas correspundentas. Las chartas èn ina basa per stimar la periclitaziun regiunala tras stemprads, senza dentant remplazzar l`ovra da referenza da la pressiun dinamica (norma SIA 261, agiunta E). La periclitaziun tras stemprads vegn calculada sin basa dad 83 periodas da stemprads d`enviern dals onns 1871 fin 2011 sco er sin basa da l`unitad da datas globala &#39;20th Century Reanalysis&#39;. Influenzas localas sco er stemprads da stad e bufs d`urizis n`èn betg vegnids resguardads per las calculaziuns. Las valurs dals bufs na dastgan perquai betg vegnir interpretadas sco valurs exactas e geograficamain precisas, ed ellas na remplazzan betg expertisas per lieus specifics. Cunzunt per lieus autalpins exponids (p.ex. Jungfraujoch) vegnan sutvalitads ils bufs.</Abstract>
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        <Abstract>La `Tranquillity Map da la Bassa Centrala svizra` mussa, nua ch`i dat, en la vischinanza da gronds abitadis da la Bassa Centrala, territoris natirals ch`èn mo levamain engrevgiads cun canera e ch`èn adattads per la recreaziun quieta. Latiers è la regiun biogeografica Bassa Centrala vegnì dividì en in raster cun ina grondezza da cellas da 100 x 100 m. Tras la calculaziun da differents facturs positivs e negativs che influenzeschan l`eveniment da ruaus e da recreaziun sur ils egls resp. sur las ureglias, è vegnida calculada ina valur da `tranquillity` per mintga cella da raster.</Abstract>
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        <Abstract>La continentalitad termica en °C è vegnida calculada sco differenza tranter la valur maximala e la valur minimala da la variaziun quotidiana da la temperatura dal fanadur, e quai durant la perioda examinada (1981-2010). La charta mussa la continentalitad termica il fanadur sin 1000 m s.m. La charta resultanta ha ina dissoluziun spaziala da 25 m x 25 m. Ella è vegnida utilisada per modellar ils stgalims d`autezza da la vegetaziun.</Abstract>
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        <Abstract>Sco basas per calcular la surfatscha han servì las valurs mesiradas a las staziuns da mesiraziun da MeteoSvizra durant la perioda 1961-1990. Sut variaziun quotidiana da la temperatura da l`aria chapeschan ins la media dal decurs da la temperatura durant il di (1961-1990). Dal decurs da la temperatura durant il di vegn selecziunada la temperatura maximala. Pervia da la radiaziun dal sulegl sa preschenta quella tar tut las staziuns il suentermezdi ca. a las 15.00. La media da la valur maximala da la variaziun quotidiana divergescha levamain da la media da la temperatura maximala dal di. La valur maximala da la variaziun quotidiana è vegnida considerada sco relevanta per la flora, perquai ch`ella è colliada cun in`auta irradiaziun dal sulegl. Las temperaturas èn vegnidas interpoladas territorialmain e verticalmain sin differents stgalims d`autezza cun agid da gradients. Supplementarmain èn vegnidas resguardadas l`exposiziun, l`irradiaziun dal sulegl sco er las surfatschas dals glatschers ed ils vonns d`aria fraida. La charta resultanta ha ina dissoluziun spaziala da 25 m x 25 m. Ella è vegnida utilisada per modellar ils stgalims d`autezza da la vegetaziun.</Abstract>
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        <Abstract>La media da la temperatura maximala da l`aria en il decurs dal di il fanadur (perioda 2070-2099). Sco basa serva la charta `Temperatura da l`aria fanadur 1981-2010`, a la quala è vegnida agiuntada la midada da la temperatura tras la midada dal clima. Per calcular la midada da la temperatura en l`avegnir è vegnì tschernì il trutg da concentraziun represchentativ RCP 2.6 cun la cumbinaziun da models DMI_HIRHAM_ECEARTH_EUR11 sco projecziun per ina pitschna midada dal clima (NCCS 2018; preparaziun da las datas tras Remund et al. 2020). La charta resultanta ha ina dissoluziun spaziala da 25 m x 25 m. Ella è vegnida utilisada per modellar ils stgalims d`autezza da la vegetaziun.</Abstract>
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        <Abstract>La media da la temperatura maximala da l`aria en il decurs dal di il fanadur (perioda 2070-2099). Sco basa serva la charta `Temperatura da l`aria fanadur 1981-2010`, a la quala è vegnida agiuntada la midada da la temperatura tras la midada dal clima. Per calcular la midada da la temperatura en l`avegnir è vegnì tschernì il trutg da concentraziun represchentativ RCP 4.5 cun la cumbinaziun da models SMHI-RCA_MPIESM_EUR44 sco projecziun per ina midada dal clima moderada (NCCS 2018; preparaziun da las datas tras Remund et al. 2020).La charta resultanta ha ina dissoluziun spaziala da 25 m x 25 m. Ella è vegnida utilisada per modellar ils stgalims d`autezza da la vegetaziun.</Abstract>
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        <Abstract>La media da la temperatura maximala da l`aria en il decurs dal di il fanadur (perioda 2070-2099). Sco basa serva la charta `Temperatura da l`aria fanadur 1981-2010`, a la quala è vegnida agiuntada la midada da la temperatura tras la midada dal clima. Per calcular la midada da la temperatura en l`avegnir è vegnì tschernì il trutg da concentraziun represchentativ RCP 8.5 cun la cumbinaziun da models CLMCOM-CCLM5_HADGEM_EUR44 sco projecziun per ina gronda midada dal clima (NCCS 2018; preparaziun da las datas tras Remund et al. 2020). La charta resultanta ha ina dissoluziun spaziala da 25 m x 25 m. Ella è vegnida utilisada per modellar ils stgalims d`autezza da la vegetaziun.</Abstract>
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        <Abstract>La charta mussa la summa da las precipitaziuns (en mm) per ils mais avrigl fin avust, calculada per la perioda 2070-2099. Sco basa serva la charta `Precipitaziuns avrigl-avust 1981-2010` ch`è vegnida deducida da las chartas da MeteoSvizra cun valurs da norma per las precipitaziuns. Per calcular la midada da la summa da las precipitaziuns en l`avegnir è vegnì tschernì il trutg da concentraziun represchentativ RCP 2.6 cun la cumbinaziun da models DMI_HIRHAM_ECEARTH_EUR11 sco projecziun per ina pitschna midada dal clima (NCCS 2018; preparaziun da las datas tras Remund et al. 2020). La charta resultanta ha ina dissoluziun spaziala da 25 m x 25 m. Ella è vegnida utilisada per modellar ils stgalims d`autezza da la vegetaziun.</Abstract>
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        <Abstract>La charta mussa l`umiditad relativa da l`aria durant il fanadur enturn las 13.30 per la perioda 1981-2010. Sco basas per calcular la surfatscha han servì las staziuns da mesiraziun da MeteoSvizra. L`umiditad relativa da l`aria è vegnida interpolada territorialmain e verticalmain sin differents stgalims d`autezza cun agid da gradients. La charta resultanta ha ina dissoluziun spaziala da 25 m x 25 m. Ella è vegnida utilisada per modellar ils stgalims d`autezza da la vegetaziun.</Abstract>
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        <Abstract>Questa charta represchenta ils stgalims d`autezza da la vegetaziun da guaud en Svizra per la perioda 1961-1990. Ils suandants stgalims d`autezza datti mo en las vals dal sid: `iperinsubric`, `collin cun fau` e `sut-/surmontan`. Per crear la charta èn ils stgalims d`autezza preschentads en Frehner et al. (2005/2009) vegnids quantifitgads e meglierads. Per quest intent èn lur cunfins sura respectivs vegnids modellads e cumbinads cun las modellaziuns da l`areal da fau sco er dals areals d`aviez (areals principals, accessorics e da relict). Sco basa per modellar ils cunfins ed ils areals èn vegnids duvrads parameters dal clima e classas da litologia.</Abstract>
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        <Title>Stgalims d`autezza 2085, sitg</Title>
        <Abstract>Questa charta represchenta ils stgalims d`autezza da la vegetaziun da guaud en Svizra per la perioda 2070-2099 sin basa da l`ipotesa ch`il clima futur saja sitg. Ils suandants stgalims d`autezza datti mo en las vals dal sid: `mediterran`, `iperinsubric`, `collin cun fau` e `montan inferiur/superiur`. Sco basa per spustar ils stgalims d`autezza vers il futur serva la charta `Stgalims d`autezza da la vegetaziun modellads per l`onn 1995`. Sco trutg da concentraziun represchentativ è vegnì tschernì RCP 8.5 cun la cumbinaziun da models CLMCOM-CCLM5_HADGEM_EUR44 sco projecziun `sitga` dal clima (NCCS 2018). Cumpareglià cun la perioda 1981-2010 fa quest model quint cun ina stgaudada media da 4,4°C (Svizra dal Nord e dal Sid) e cun ina reducziun da las precipitaziuns per 17,0% (Svizra dal nord) resp. per 24,9% (Svizra dal Sid) per ils mais d`avrigl fin avust, che vegnan resguardads sco ils pli relevants per il clima dals bostgs (Remund 2020). Il cunfin natiral superiur dal guaud è vegnì modellà cun ina procedura analoga (Könz et al. 2021). --- Funtauna: Zischg et al. (subm.)</Abstract>
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        <Abstract>Questa charta represchenta ils stgalims d`autezza da la vegetaziun da guaud en Svizra per la perioda 2070-2099 sin basa da l`ipotesa d`in clima futur main sitg. Ils suandants stgalims d`autezza datti mo en las vals dal sid: `mediterran`, `iperinsubric`, `collin cun fau` e `montan inferiur/superiur`. Sco basa per spustar ils stgalims d`autezza vers il futur serva la charta `Stgalims d`autezza da la vegetaziun modellads per l`onn 1995`. Dals trutgs da concentraziun represchentativs è vegnì tschernì RCP 4.5 cun la cumbinaziun da models SMHI-RCA_MPIESM_EUR44 sco projecziun `main sitga` dal clima (NCCS 2018). Cumpareglià cun la perioda 1981-2010 fa quest model quint cun ina stgaudada media dad 1,8°C (Svizra dal Nord) resp. da 2,3°C (Svizra dal Sid) e cun ina reducziun da las precipitaziuns per 4,0% (Svizra dal nord) resp. per 0,5% (Svizra dal Sid) per ils mais d`avrigl fin avust, che vegnan resguardads sco ils pli relevants per il clima dals bostgs (Remund 2020). Il cunfin natiral superiur dal guaud è vegnì modellà cun ina procedura analoga (Könz et al. 2021). --- Funtauna: Zischg et al. (subm.)</Abstract>
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        <Abstract>Durant il temp da vegetaziun han ils bostgs savens a disposiziun damain aua: -La purschida d`aua durant il temp da vegetaziun è decisiva per la creschientscha e per la vitalitad dals guauds. La disponibladad da l`aua po vegnir calculada or da la differenza tranter las precipitaziuns e la svapuraziun potenziala. Quai è la bilantscha d`aua climatica. Amplifitgada per l`accumulaziun en il terren resulta la bilantscha d`aua d`in lieu. -La bilantscha d`aua d`in lieu ha in stretg connex cun l`existenza dals bostgs, cun lur vitalitad e cun lur creschientscha. -Las spezias da bostgs han pretensiuns differentas areguard la purschida d`aua. Entant che ruvers èn cuntents cun pauca aua, dovran pigns cleramain dapli aua durant il temp da vegetaziun. -Tendenza: repetiziun ed extensiun dals territoris mellens fin cotschens s`augmentan en la perioda 1981-2018. Perioda 1981-2018, avrigl fin avust, dissoluziun spaziala 250m x 250m. Funtauna: Remund et al. (2016).</Abstract>
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        <Abstract>Als bostgs stat adina pli savens a disposiziun memia pauca aua: -La vegetaziun ed il terren dattan aua a l`atmosfera: pli chauda e pli sitga che l`aria è, e pli blera aua che quai è. Plantas svapureschan aua sur lur feglia. L`evapotranspiraziun è la summa da l`aua che vegn dada giu a l`atmosfera. -L`evapotranspiraziun actuala (ETa) dependa da la disponibladad d`aua, quai vul dir da la quantitad da precipitaziuns sco er da l`abilitad dals funs d`accumular l`aua da precipitaziuns. -L`evapotranspiraziun potenziala (ETp) è la quantitad d`aua che vegniss dada giu a l`atmosfera, sch`i stess a disposiziun avunda aua. -Sche la relaziun ETa/ETp croda sut ina valur da 0,8, stoi vegnir fatg quint cun donns pervia da setgira, perquai che las sfessas da la feglia èn alura savens serradas ed ils bostgs reduceschan la fotosintesa. -En territoris blau clers ed en spezial en territoris blau stgirs na stoi betg vegnir fatg quint cun disturbis. -En territoris marcads cun mellen fin cotschen stoi vegnir fatg quint cun donns dals bostgs pervia da setgira, il pli fitg en ils secturs cotschen vin. -Tendenza: repetiziun ed extensiun dals territoris mellens fin cotschens s`augmentan en la perioda 1981-2018. Perioda 1981-2018, avrigl fin avust, dissoluziun spaziala 250m x 250m. Funtauna: Remund et al. (2016).</Abstract>
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        <Abstract>Reservats da guaud èn da princip surfatschas protegidas en moda permanenta che servan a la diversitad ecologica e biologica dal guaud. D`ina vart pussibiliteschan els al guaud sco sistem ecologic da sa sviluppar en moda cumplettamain natirala areguard il spazi ed areguard il temp (protecziun da la dinamica natirala en uschenumnads reservats da guaud natiral). Da l`autra vart servan els a mantegnair spazis da viver spezials (habitats) per tschertas spezias. Per quai dovri mesiras da promoziun sistematicas (en uschenumnads &#39;reservats da guaud spezials&#39; resp. en &#39;reservats cun intervenziuns spezialas&#39;). Preschentads vegnan ils perimeters dals reservats che pon er cuntegnair surfatschas betg forestalas. Cumplementarmain annunzian intgins chantuns er surfatschas da guaud, da las qualas la protecziun è reglada en disposiziuns (guauds en territori da protecziun da la natira, zonas umidas, guauds da palì e.u.v.). Questas unitads da datas vegnan er represchentadas. La cumpetenza per installar reservats da guaud han ils chantuns. Ils chantuns furneschan al UFAM las datas geograficas (geodatas) da lur reservats da guaud. Quel fa cun quellas alura ina statistica naziunala. Ils guauds protegids èn classifitgads tenor l`agiunta 2 da la Resoluziun da Vienna 4 da la Conferenza ministeriala davart la protecziun dals guauds en Europa. Quella prevesa 3 categorias (1.1 naginas intervenziuns, 1.2 intervenziuns minimalas, 1.3 promoziun da la biodiversitad cun intervenziuns activas), entant che l`economia forestala svizra lavura cun 2 categorias (reservat da guaud natiral e reservat da guaud spezial). Ils reservats da guaud spezial svizzers vegnan attribuids a la categoria 1.3, entant ch`ils reservats da guaud natiral appartegnan a la categoria 1.1 u 1.2 tut tenor la cunvegna. Ils guauds protegids tras ordinaziun e disposiziun vegnan classifitgads tenor cundiziuns en il conclus da protecziun. L`attribuziun da las surfatschas da guaud protegidas a las 3 categorias da la Resoluziun da Vienna è chaussa dals chantuns respectivs.</Abstract>
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        <Abstract>L`inventari dals donns da stemprà Lothar da la Confederaziun aveva sco finamira da registrar cumplettamain ed en moda unitara per tut la Svizra ils donns totals e sparpagliads en il guaud. Las suandantas caracteristicas da registraziun e cundiziuns generalas èn vegnidas formuladas: Surfatschas da donns totals: surfatscha da guaud destruida cun in grad da cuvrida da la populaziun forestala restanta da 0,2 (20 %) *), independentamain dal fatg, tge grad da cuvrida ch`il guaud aveva là avant. Surfatschas da donns sparpagliads: surfatscha da guaud destruida per part cun ina populaziun forestala restanta en la stresa superiura e cun in grad da cuvrida da tranter 0,2 e 0,6*); surfatschas cun grads da cuvrida da &gt; 0,6 na valan betg pli sco surfatschas donnegiadas dal stemprà. Exempels cun problems da cunfinar las surfatschas da donns totals e las surfatschas da donns sparpagliads cun propostas da soluziun respectivas (lingias da cunfin cotschnas sin folias transparentas) èn preschentads en il chapitel 8. Surfatschas da guaud che avevan gia avant il donn in grad da cuvrida pitschen (p.ex. guauds da pastgira cun ina populaziun forestala lucca) han fatg pretensiuns spezialas a l`interpretaziun da las fotografias or da l`aria. Sco meds d`agid per stimar ils grads da cuvrida han servì ils exempels en il chapitel 7.5. Surfatschas minimalas: Per surfatscha singula registrada 1,0 hectaras. La controlla tar la determinaziun da l`effectiv è vegnida fatga cun ina schablona (folia) per differentas scalas da las fotografias or da l`aria. Gruppaziun da surfatschas: Sche surfatschas da donns da differents geners eran ina sper l`autra, ha la surfatscha totala stuì esser pli gronda che 1 hectara. La surfatscha parziala po esser en il cas singul pli pitschna che 1 hectara.</Abstract>
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        <Abstract>Inventari federal dals donns chaschunads dal stemprà Vivian il favrer 1990. Registraziun da las surfatschas da donns totals vi dal guaud. Caracteristicas da la registraziun: Surfatscha da donns totals: surfatscha da guaud destruida cun in grad da cuvrida da la populaziun forestala restanta da &lt;= 0,2 (20 %), independentamain dal fatg, tge grad da cuvrida ch`il guaud aveva là avant. Surfatscha minimala: Per surfatscha singula registrada 0,2 hectaras. Caracteristicas dal lieu: Sco valur forestala impurtanta vegnan registradas per mintga surfatscha da donns l`inclinaziun, l`autezza e l`exposiziun da la spunda. Unitads da registraziun e d`evaluaziun: L`unitad da registraziun la pli pitschna è la surfatscha donnegiada dal stemprà, l`unitad d`evaluaziun la pli pitschna è la vischnanca politica. Per l`attribuziun territoriala da questas duas unitads vegnan surpigliadas da S+T las datas digitalisadas dals cunfins da las vischnancas.</Abstract>
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      <Abstract>La charta mussa ils trajects d`auas che vegnan mesirads periodicamain sut la direcziun dal UFAM. La mesiraziun vegn fatga per regla mintga 10 onns u suenter grondas auas grondas che han chaschunà midadas morfologicas impurtantas. Las finamiras da la mesiraziun periodica èn: - constatar ad ura tendenzas morfologicas (erosiun, accumulaziun) e lur consequenzas per la stabilitad d`ovras da protecziun u per la capacitad da deflussiun; - metter a disposiziun serias temporaras da blers onns davart la midada dals letgs da curs d`aua sco basa per quantifitgar il reschim da sediments; - metter a disposiziun datas actualas per planisar e per evaluar ils privels. Las datas da mesiraziun vegnan administradas da la partiziun &#39;prevenziun cunter privels&#39;, secziun &#39;management da las ristgas&#39;.</Abstract>
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        <Abstract>La charta mussa ils trajects d`auas che vegnan mesirads periodicamain sut la direcziun dal UFAM. La mesiraziun vegn fatga per regla mintga 10 onns u suenter grondas auas grondas che han chaschunà midadas morfologicas impurtantas. Las finamiras da la mesiraziun periodica èn: - constatar ad ura tendenzas morfologicas (erosiun, accumulaziun) e lur consequenzas per la stabilitad d`ovras da protecziun u per la capacitad da deflussiun; - metter a disposiziun serias temporaras da blers onns davart la midada dals letgs da curs d`aua sco basa per quantifitgar il reschim da sediments; - metter a disposiziun datas actualas per planisar e per evaluar ils privels. Las datas da mesiraziun vegnan administradas da la partiziun &#39;prevenziun cunter privels&#39;, secziun &#39;management da las ristgas&#39;.</Abstract>
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        <Abstract>La charta mussa ils trajects d`auas che vegnan mesirads periodicamain sut la direcziun dal UFAM. La mesiraziun vegn fatga per regla mintga 10 onns u suenter grondas auas grondas che han chaschunà midadas morfologicas impurtantas. Las finamiras da la mesiraziun periodica èn: - constatar ad ura tendenzas morfologicas (erosiun, accumulaziun) e lur consequenzas per la stabilitad d`ovras da protecziun u per la capacitad da deflussiun; - metter a disposiziun serias temporaras da blers onns davart la midada dals letgs da curs d`aua sco basa per quantifitgar il reschim da sediments; - metter a disposiziun datas actualas per planisar e per evaluar ils privels. Las datas da mesiraziun vegnan administradas da la partiziun &#39;prevenziun cunter privels&#39;, secziun &#39;management da las ristgas&#39;.</Abstract>
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      <Abstract>Asils da selvaschina han l`intent da proteger tscherts mammals ed utschels sco er lur biotops. Ils 43 asils federals da selvaschina registrads sa basan sin l`art. 11 da la Lescha da chatscha. Sports d`enviern dastgan vegnir fatgs mo sin rutas marcadas. Per ils sportists d`enviern valan uschia las medemas restricziuns d`access sco en las zonas da paus per la selvaschina giuridicamain liantas, nua ch`igl è obligatoric da star sin ina tscherta ruta. Entaifer las zonas da paus per la selvaschina ed ils asils da selvaschina giuridicamain liants dastgan ins chaminar mo sin las rutas e sendas permessas ch`èn inditgadas sin la charta. Betg inditgadas èn loipas (da passlung) preparadas, sendas da viandar l`enviern sco er vias rumidas da la naiv u charrablas l`enviern. Quellas dastgan natiralmain vegnir duvradas dals sportists d`enviern. Runals u pendicularas èn inditgadas en asils (federals) da selvaschina. Els inditgeschan, nua ch`i sa chattan infrastructuras che dastgan vegnir duvradas dals sportists d`enviern ensemen cun las pistas respectivas. Las pistas n`èn betg inditgadas. La campagna &#39;Respecta tes cunfins - er en la natira&#39; s`engascha per la protecziun da la selvaschina e vul er render enconuschentas a la populaziun las zonas da paus per la selvaschina.</Abstract>
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        <Abstract>Asils da selvaschina han l`intent da proteger tscherts mammals ed utschels sco er lur biotops. Ils 43 asils federals da selvaschina registrads sa basan sin l`art. 11 da la Lescha da chatscha. Sports d`enviern dastgan vegnir fatgs mo sin rutas marcadas. Per ils sportists d`enviern valan uschia las medemas restricziuns d`access sco en las zonas da paus per la selvaschina giuridicamain liantas, nua ch`igl è obligatoric da star sin ina tscherta ruta. Entaifer las zonas da paus per la selvaschina ed ils asils da selvaschina giuridicamain liants dastgan ins chaminar mo sin las rutas e sendas permessas ch`èn inditgadas sin la charta. Betg inditgadas èn loipas (da passlung) preparadas, sendas da viandar l`enviern sco er vias rumidas da la naiv u charrablas l`enviern. Quellas dastgan natiralmain vegnir duvradas dals sportists d`enviern. Runals u pendicularas èn inditgadas en asils (federals) da selvaschina. Els inditgeschan, nua ch`i sa chattan infrastructuras che dastgan vegnir duvradas dals sportists d`enviern ensemen cun las pistas respectivas. Las pistas n`èn betg inditgadas. La campagna &#39;Respecta tes cunfins - er en la natira&#39; s`engascha per la protecziun da la selvaschina e vul er render enconuschentas a la populaziun las zonas da paus per la selvaschina.</Abstract>
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      <Abstract>Ils animals selvadis dovran refugis, nua ch`els na vegnan betg disturbads. La determinaziun da zonas da paus per la selvaschina serva ad evitar disturbis memia gronds tenor l`art. 7 al. 4 LChP sco resposta a l`augment da l`utilisaziun da temp liber. Oz datti zonas da paus per la selvaschina e territoris protegids giuridicamain liants ch`èn vegnids determinads sin basa d`in process legislativ (dretg da chatscha chantunal, planisaziun communala da zonas e.u.v.) sco er territoris recumandads. Entaifer las zonas da paus per la selvaschina ed ils asils da selvaschina giuridicamain liants dastgan ins chaminar mo sin las rutas e sendas permessas ch`èn inditgadas sin la charta. Betg inditgadas èn loipas (da passlung) preparadas, sendas da viandar l`enviern sco er vias rumidas da la naiv u charrablas l`enviern. Quellas dastgan natiralmain vegnir duvradas dals sportists d`enviern. En zonas da paus per la selvaschina recumandadas ston las rutas e sendas permessas vegnir chapidas sco recumandaziuns. Il stadi da las lavurs en ils chantuns è actualmain fitg different, perquai ha l`unitad da datas largias. La charta vegn actualisada almain ina giada l`onn (il cumenzament da l`enviern). Resguardai per plaschair las infurmaziuns generalas e las midadas (p.ex. adattaziuns dal perimeter) che n`han anc betg pudì vegnir resguardadas en la charta. La campagna &#39;Respecta tes cunfins - er en la natira&#39; s`engascha per la protecziun da la selvaschina e vul er render enconuschentas a la populaziun las zonas da paus per la selvaschina.</Abstract>
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        <Abstract>Ils animals selvadis dovran refugis, nua ch`els na vegnan betg disturbads. La determinaziun da zonas da paus per la selvaschina serva ad evitar disturbis memia gronds tenor l`art. 7 al. 4 LChP sco resposta a l`augment da l`utilisaziun da temp liber. Oz datti zonas da paus per la selvaschina e territoris protegids giuridicamain liants ch`èn vegnids determinads sin basa d`in process legislativ (dretg da chatscha chantunal, planisaziun communala da zonas e.u.v.) sco er territoris recumandads. Entaifer las zonas da paus per la selvaschina ed ils asils da selvaschina giuridicamain liants dastgan ins chaminar mo sin las rutas e sendas permessas ch`èn inditgadas sin la charta. Betg inditgadas èn loipas (da passlung) preparadas, sendas da viandar l`enviern sco er vias rumidas da la naiv u charrablas l`enviern. Quellas dastgan natiralmain vegnir duvradas dals sportists d`enviern. En zonas da paus per la selvaschina recumandadas ston las rutas e sendas permessas vegnir chapidas sco recumandaziuns. Il stadi da las lavurs en ils chantuns è actualmain fitg different, perquai ha l`unitad da datas largias. La charta vegn actualisada almain ina giada l`onn (il cumenzament da l`enviern). Resguardai per plaschair las infurmaziuns generalas e las midadas (p.ex. adattaziuns dal perimeter) che n`han anc betg pudì vegnir resguardadas en la charta. La campagna &#39;Respecta tes cunfins - er en la natira&#39; s`engascha per la protecziun da la selvaschina e vul er render enconuschentas a la populaziun las zonas da paus per la selvaschina.</Abstract>
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        <Abstract>Il 1. da november 1992 è entrada en vigur la Lescha federala dals 24 da schaner 1991 davart la protecziun da las auas (LPAuas) che cuntegna er disposiziuns davart las quantitads d`aua restanta. Tenor ils artitgels 80 ss. LPAuas ston trajects d`aua restanta existents vegnir sanads sin ordinaziun da las autoritads, uschenavant che quai è pussaivel. Sco emprima incumbensa en vista a questa sanaziun han ils chantuns stuì far in inventari da las prelevaziuns d`aua existentas ed inoltrar quest inventari a la Confederaziun. Sin questa basa giuditgeschan ils chantuns las prelevaziuns d`aua ch`èn registradas en l`inventari e decidan, sche ed en tge dimensiun ch`ina sanaziun è necessaria. Ils resultats da lur retschertgas integreschan els en in rapport e suttamettan quest rapport medemamain a la Confederaziun. Per avair ina survista da l`execuziun da la LPAuas en il sectur da l`aua restanta e da la sanaziun e per pudair infurmar la publicitad ed auters posts interessads, vegnan las datas davart las prelevaziuns d`aua, ch`ils chantuns han inoltrà, preschentadas en ina carta naziunala d`aua restanta (scala 1:200`000).</Abstract>
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        <Abstract>Il 1. da november 1992 è entrada en vigur la Lescha federala dals 24 da schaner 1991 davart la protecziun da las auas (LPAuas) che cuntegna er disposiziuns davart las quantitads d`aua restanta. Tenor ils artitgels 80 ss. LPAuas ston trajects d`aua restanta existents vegnir sanads sin ordinaziun da las autoritads, uschenavant che quai è pussaivel. Sco emprima incumbensa en vista a questa sanaziun han ils chantuns stuì far in inventari da las prelevaziuns d`aua existentas ed inoltrar quest inventari a la Confederaziun. Sin questa basa giuditgeschan ils chantuns las prelevaziuns d`aua ch`èn registradas en l`inventari e decidan, sche ed en tge dimensiun ch`ina sanaziun è necessaria. Ils resultats da lur retschertgas integreschan els en in rapport e suttamettan quest rapport medemamain a la Confederaziun. Per avair ina survista da l`execuziun da la LPAuas en il sectur da l`aua restanta e da la sanaziun e per pudair infurmar la publicitad ed auters posts interessads, vegnan las datas davart las prelevaziuns d`aua, ch`ils chantuns han inoltrà, preschentadas en ina carta naziunala d`aua restanta (scala 1:200`000).</Abstract>
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        <Abstract>La Lescha federala davart la protecziun da la natira e da la patria (CS 451) definescha, suenter la revisiun dal 1. da december 2007, trais categorias da parcs d`impurtanza naziunala: parcs naziunals, parcs natirals regiunals e parcs natirals d`aventura. Tut tenor il stadi dal project pon las regiuns pertutgadas dumandar il label &#39;Candidatura&#39; per stabilir in parc u il label &#39;Parc&#39; (sco marca protegida) per manar il parc. Parcs d`impurtanza naziunala gidan a proteger ed ad augmentar la valur da spazis da viver natirals extraordinaris. A medem temp sustegnan ils parcs il svilup economic d`ina regiun. L`unitad da datas &#39;Parcs&#39; cuntegna supplementarmain ils projects da parcs ch`èn annunziads tar il UFAM sco er il territori da protecziun &#39;Parc naziunal svizzer&#39; ch`è protegì tenor la Lescha federala dals 19 da december 1980 davart il Parc naziunal (CS 454).</Abstract>
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        <Abstract>La rait ecologica naziunala REN è vegnida elavurada en stretga collavuraziun cun ils posts chantunals spezialisads per la protecziun da la natira e da la cuntrada. I sa tracta d`in rapport tecnic/scientific che mussa la cuntrada da la Svizra ord vista ecologica. Sin chartas a la scala 1:500`000 ed 1:100`000 preschenta el tant las fragmentaziuns sco er ils elements da colliaziun dals spazis da viver. Contemplada na vegn betg mo la situaziun actuala, er il potenzial da la cuntrada vegn resguardà. Questa visiun cumplessiva e progressiva porscha in maletg cumplet da las grondas raits ecologicas dal pajais. Las chartas da las raits specificas mussan - per las tschintg raits specificas - ils territoris centrals, ils territoris d`extensiun sco er ils continuums ed ils corridors. La situaziun da colliaziun per mintga rait specifica è preschentada en in`ulteriura unitad da chartas.</Abstract>
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        <Abstract>La rait ecologica naziunala REN è vegnida elavurada en stretga collavuraziun cun ils posts chantunals spezialisads per la protecziun da la natira e da la cuntrada. I sa tracta d`in rapport tecnic/scientific che mussa la cuntrada da la Svizra ord vista ecologica. Sin chartas a la scala 1:500`000 ed 1:100`000 preschenta el tant las fragmentaziuns sco er ils elements da colliaziun dals spazis da viver. Contemplada na vegn betg mo la situaziun actuala, er il potenzial da la cuntrada vegn resguardà. Questa visiun cumplessiva e progressiva porscha in maletg cumplet da las grondas raits ecologicas dal pajais. Las chartas da las raits specificas mussan - per las tschintg raits specificas - ils territoris centrals, ils territoris d`extensiun sco er ils continuums ed ils corridors. La situaziun da colliaziun per mintga rait specifica è preschentada en in`ulteriura unitad da chartas.</Abstract>
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        <Abstract>La rait ecologica naziunala REN è vegnida elavurada en stretga collavuraziun cun ils posts chantunals spezialisads per la protecziun da la natira e da la cuntrada. I sa tracta d`in rapport tecnic/scientific che mussa la cuntrada da la Svizra ord vista ecologica. Sin chartas a la scala 1:500`000 ed 1:100`000 preschenta el tant las fragmentaziuns sco er ils elements da colliaziun dals spazis da viver. Contemplada na vegn betg mo la situaziun actuala, er il potenzial da la cuntrada vegn resguardà. Questa visiun cumplessiva e progressiva porscha in maletg cumplet da las grondas raits ecologicas dal pajais. Las chartas da las raits specificas mussan - per las tschintg raits specificas - ils territoris centrals, ils territoris d`extensiun sco er ils continuums ed ils corridors. La situaziun da colliaziun per mintga rait specifica è preschentada en in`ulteriura unitad da chartas.</Abstract>
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        <Abstract>L`unitad da datas represchenta ils lieus da las staziuns da la rait da mesiraziun da basa da la partiziun Idrologia dal UFAM. Ella cuntegna tut las staziuns actualas che vegnan publitgadas sin la pagina d`internet dal UFAM. La rait da mesiraziun da basa cumpiglia oz circa 260 staziuns da mesiraziun da las auas da surfatscha. Ultra dal livel da l`aua en ils lais vegn eruida en 200 lieus la deflussiun dals flums. 90 % da tut las staziuns disponan d`ina consultaziun automatica a distanza.</Abstract>
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        <Abstract>Suenter sia recolonisaziun l`onn 1906 viva il capricorn alpin en diversas colonias da differenta dimensiun en las Alps ed en il Giura. En singulas colonias ha la creschientscha dals effectivs gì consequenzas negativas per autras spezias e per la vegetaziun, uschia ch`i vegnan prendidas mesiras da regulaziun. Las prescripziuns davart las planisaziuns da la reducziun dals effectivs da capricorns sa basan sin la Lescha federala dals 20 da zercladur 1986 davart la chatscha e la protecziun dals mamifers e dals utschels selvadis. Las colonias vegnan registradas tenor las prescripziuns davart las relevaziuns dals effectivs da l`Ordinaziun dals 30 d`avrigl 1990 davart la regulaziun dals effectivs da capricorns e furman, ensemen cun las relevaziuns dals effectivs, la basa per planisar la reducziun dals effectivs.</Abstract>
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        <Abstract>Per differentas spezias d`utschels da l`aua migrants ha la Svizra ina impurtanza speziala sco lieu per passentar l`enviern e per pussar. En enconuschientscha da questa impurtanza ha il Cussegl federal suttascrit l`onn 1974 la Convenziun davart las zonas umidas d`impurtanza naziunala. Questa convenziun è vegnida concludida l`onn 1971 a Ramsar (Convenziun da Ramsar). L`Assamblea federala l`ha ratifitgada l`onn 1975. L`onn 1976 è vegnì elavurà per la Svizra in inventari dals reservats d`utschels da l`aua d`impurtanza internaziunala sin basa da criteris anteriurs. La Staziun ornitologica svizra Sempach ha preschentà l`onn 1995 la segunda versiun revedida da quest inventari inclusiv ils objects d`impurtanza naziunala. Tenor l`artitgel 11 da la nova Lescha federala davart la chatscha e la protecziun dals mamifers e dals utschels selvadis (LChP) è la Confederaziun obligada da determinar reservats d`utschels da l`aua e d`utschels migrants d`impurtanza internaziunala. Suenter las revisiuns dals onns 1992, 2001, 2009, 2015 e 2023 cuntegna l`inventari actual ils territoris ils pli impurtants ch`èn cuntegnids en l`inventari da la Staziun ornitologica svizra. Da quels èn 10 d`impurtanza internaziunala e 25 d`impurtanza naziunala.</Abstract>
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        <Abstract>Cuntradas da palì èn cuntradas natiralas ch`èn caracterisadas en moda speziala tras palids e che cuntegnan plinavant er elements natirals e culturals remartgabels. Per differentas spezias d`animals e da plantas èn ellas ils ultims biotops restads. L`inventari scientific da las cuntradas da palì è vegnì elavurà ils onns 1987 fin 1990 da la firma Hintermann &amp; Weber SA per incumbensa dal DFI. Tenor l`art. 23b da la Lescha federala dal 1. da fanadur 1966 davart la protecziun da la natira e da la patria (LPNP) designescha il Cussegl federal, resguardond l`urbanisaziun e l`utilisaziun existenta, las cuntradas da palì da bellezza particulara e d`impurtanza naziunala ch`èn degnas da vegnir protegidas e determinescha lur situaziun. En quest connex collavura el stretgamain cun ils chantuns che consulteschan da lur vart ils proprietaris dals bains immobigliars pertutgads. L`onn 1996 ha il Cussegl federal mess en vigur l`Ordinaziun davart las cuntradas da palì e - sco agiunta - l`inventari federal cun 88 objects. In`emprima revisiun hai dà l`onn 2001 sin dumonda dal chantun Vad, ina segunda l`onn 2004 cun l`inscripziun definitiva da l`object Grimsel e trais ulteriuras ils onns 2007, 2015 e 2017. Actualmain èn en vigur 89 objects.</Abstract>
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        <Abstract>Asils federals da selvaschina existan dapi l`onn 1875. Els avevan l`intent d`augmentar ils effectivs da chamutschs, da tschiervs e da chavriels sco er da capricorns (selvaschina d`ungla) ch`eran daventads rars da quel temp pervia da la chatscha e pervia da la concurrenza tras il muvel. Oz è la situaziun caracterisada d`ina vart tras gronds effectivs da selvaschina d`ungla, per part effectivs excessivs, e tras ils donns che quests effectivs chaschunan, da l`autra vart tras la reducziun da spezias sensiblas sco la giaglina da taus e da draussa, la pernisch da gonda, la pernisch grischa e la lieur brina. Il 1. d`avrigl 1988 è entrada en vigur la Lescha federala dals 20 da zercladur 1986 davart la chatscha e la protecziun dals mamifers e dals utschels selvadis (LChP). Uschia è er vegnida instradada la revisiun da l`Ordinaziun davart ils asils da selvaschina da l`onn 1962. Quests dus decrets han oz la finamira da reglar ils effectivs da tschiervs, chavriels, chamutschs e capricorns sco er da proteger e da promover las spezias raras e lur biotops. L`inventari cuntegna 42 objects ch`èn per part vegnids modifitgads levamain dapi l`onn 1992.</Abstract>
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        <Abstract>Las palids autas tutgan tar ils biotops ils pli sensibels da la Svizra e sa diminueschan fermamain. Oz existan anc var 10 fin 20 % da l`effectiv oriund. L`inventari scientific da las palids autas e transiziunalas è vegnì elavurà ils onns 1978 fin 1984 da la partiziun per la cuntrada dal WSL (Institut federal per la perscrutaziun da guaud, naiv e cuntrada) per incumbensa da la Pro Natura Helvetica. Tenor l`art. 18a da la Lescha federala dal 1. da fanadur 1966 davart la protecziun da la natira e da la patria (LPNP) (en vigur dapi il 1. da favrer 1988) designescha il Cussegl federal ils biotops d`impurtanza naziunala, fixescha la situaziun da quests biotops e determinescha las finamiras da protecziun. Quai fa el suenter avair tadlà ils chantuns. Sco emprim inventari federal tenor l`art. 18a LPNP ha il Cussegl federal mess en vigur l`onn 1991 l`Inventari federal da las palids autas e transiziunalas d`impurtanza naziunala cun 514 objects. L`onn 2003 hai dà ina cumplettaziun cun ina 2. seria. Ils onns 2007,2017 e 2025 è l`inventari vegnì revedì, uschia ch`el cumpiglia actualmain 552 objects.</Abstract>
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        <Abstract>Las palids planivas èn restanzas da la cuntrada natirala e cultivada oriunda che sa diminueschan pli e pli. En ellas vivan biocenosas da plantas e d`animals fitg assimilads a las relaziuns cun in grond dumber da spezias da plantas e d`animals periclitadas. L`inventari scientific da las palids planivas è vegnì elavurà ils onns 1987 fin 1990 d`ina cuminanza da lavur per incumbensa dal DFI. Tenor l`art. 18a da la Lescha federala dal 1. da fanadur 1966 davart la protecziun da la natira e da la patria (LPNP) designescha il Cussegl federal ils biotops d`impurtanza naziunala, fixescha la situaziun da quests biotops e determinescha las finamiras da protecziun. Quai fa el suenter avair tadlà ils chantuns. L`onn 1994 ha il Cussegl federal mess en vigur l`Ordinaziun davart las palids planivas e - sco agiunta - l`inventari federal cun in`emprima seria da 728 objects. Ina segunda seria cun 364 objects è suandada l`onn 1997 e la terza seria finala cun 71 objects l`onn 1998. Intgins objects èn vegnids revedids ils onns 2001, 2004, 2007, 2017, 2021 e 2025. Actualmain èn en vigur 1371 objects.</Abstract>
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        <Abstract>Tenor l`artitgel 5 da la Lescha federala dal 1. da fanadur 1966 davart la protecziun da la natira e da la patria (LPNP) sto il Cussegl federal elavurar inventaris cun objects d`impurtanza naziunala (inventaris federals). Quai fa el cun consultar ils chantuns. L`Inventari federal da las cuntradas e dals monuments natirals d`impurtanza naziunala (IFC) è l`emprim inventari tenor la LPNP. Avant avevan organisaziuns privatas edì per l`emprima giada l`onn 1963 l`Inventari da las cuntradas e dals monuments natirals d`impurtanza naziunala degns da vegnir protegids. Quest inventari è lura vegnì cumplettà e repassà periodicamain. Il IFC è vegnì mess en vigur en etappas. Fin ussa ha il Cussegl federal approvà quatter parts: ina 1. seria l`onn 1977 cun 65 objects, ina 2. seria l`onn 1983 cun 55 objects e 5 objects revedids, ina 3. seria l`onn 1996 cun 33 objects e 10 objects revedids, ina 4. seria l`onn 1998 cun 9 objects e 15 objects revedids. A chaschun da la revisiun 2017 è vegnì realisà in barat da las surfatschas tranter ils objects 1605 e 1606.</Abstract>
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        <Abstract>Sco biotops natirals en il sectur d`inundaziun da las auas sa diminueschan las zonas umidas pli e pli. Il matg 1981 ha il DFI surdà a l`Institut federal da retschertgas forestalas (oz WSL) l`incumbensa d`elavurar in inventari scientific da las zonas umidas. Quest inventari è vegnì elavurà en l`institut da la gruppa per la perscrutaziun da la vegetaziun. Tenor l`art. 18a da la Lescha federala dal 1. da fanadur 1966 davart la protecziun da la natira e da la patria (LPNP) designescha il Cussegl federal ils biotops d`impurtanza naziunala, fixescha la situaziun da quests biotops e determinescha las finamiras da protecziun (art. 18a LPNP ch`è en vigur dapi il 1. da favrer 1988). Quai fa el suenter avair tadlà ils chantuns. Sco segund inventari federal tenor l`art. 18a LPNP ha il Cussegl federal mess en vigur l`onn 1992 l`Inventari federal da las zonas umidas cun 169 objects. Ils onns 2001, 2003, 2007 e 2017 hai dà revisiuns. Ils onns 1995 fin 1997 è vegnì elavurà - sco inventari scientific - l`Inventari dals avantglatschers e da las planiras alluvialas alpinas (ITAPA) sco basa da l`emprima cumplettaziun. Actualmain èn en vigur 326 objects. Plinavant cuntegna l`agiunta 2 tut en tut 27 objects, dals quals ils perimeters n`èn betg anc rectifitgads definitivamain. Fin ch`igl è decidì d`als integrar en l`agiunta 1, sa drizza lur protecziun tenor l`artitgel 29 alinea 1 litera a da l`Ordinaziun davart la protecziun da la natira e da la patria (OPNP) e tenor l`artitgel 7 da l`Ordinaziun da las zonas umidas.</Abstract>
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        <Abstract>En Svizra vivan oz 19 spezias d`amfibis - bunamain tuttas èn sin la Glista cotschna da las spezias d`animals periclitadas. La surfatscha da las zonas umidas sco biotop dals amfibis è sa reducida entaifer ils ultims 100 onns a main ch`in dieschavel. Ils biotops restants duessan perquai vegnir preservads. Sco auas per fregar preferescha la gronda part da las spezias auas pitschnas fixas sco puzs e paltauns. Ultra da puzs pli pitschens e da gronds cumplexs da zonas umidas furman foss da glera e d`arschiglia ina gronda part da l`inventari (circa in tschintgavel da tut ils objects). En il decurs da l`utilisaziun èn els sa sviluppads a lieus quasi-natirals degns da vegnir protegids. Ils objects movibels cumpiglian foss utilisads, entaifer ils quals duai vegnir mantegnida la premissa dinamica per preservar ils effectivs d`amfibis existents. Sco quart inventari federal tenor l`art. 18a LPNP ha il Cussegl federal mess en vigur l`onn 2001 l`Inventari federal da las plazzas da fregar per amfibis cun 701 objects. Ils onns 2003, 2007, 2017 e 2025 è quel vegnì revedì. Actualmain èn en vigur 969 objects (873 objects fixs e 96 objects movibels). Plinavant cuntegna l`agiunta 3 tut en tut 25 objects, dals quals ils perimeters n`èn betg anc rectifitgads definitivamain. Fin ch`igl è decidì d`als integrar en l`agiunta 1 u 2, sa drizza lur protecziun tenor l`artitgel 29 alinea 1 litera a da l`Ordinaziun davart la protecziun da la natira e da la patria (OPNP) e tenor l`artitgel 10 da l`Ordinaziun davart la protecziun da las plazzas da fregar per amfibis d`impurtanza naziunala (OPFA).</Abstract>
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        <Abstract>En Svizra vivan oz 19 spezias d`amfibis - bunamain tuttas èn sin la Glista cotschna da las spezias d`animals periclitadas. La surfatscha da las zonas umidas sco biotop dals amfibis è sa reducida entaifer ils ultims 100 onns a main ch`in dieschavel. Ils biotops restants duessan perquai vegnir preservads. Sco auas per fregar preferescha la gronda part da las spezias auas pitschnas fixas sco puzs e paltauns. Ultra da puzs pli pitschens e da gronds cumplexs da zonas umidas furman foss da glera e d`arschiglia ina gronda part da l`inventari (circa in tschintgavel da tut ils objects). En il decurs da l`utilisaziun èn els sa sviluppads a lieus quasi-natirals degns da vegnir protegids. Ils objects fixs (AM_L) èn dividids en dus differents secturs: Il sectur A è suttamess a la protecziun da la natira. Il sectur B cumpiglia il sectur pli stretg dals biotops sin la terra e las zonas da plimatsch. Per ordinari èn quai surfatschas utilisadas da l`agricultura e da la selvicultura. Ils objects movibels (AM_G) cumpiglian foss utilisads, entaifer ils quals duai vegnir mantegnida la premissa dinamica per preservar ils effectivs d`amfibis existents. Sco quart inventari federal tenor l`art. 18a LPNP ha il Cussegl federal mess en vigur l`onn 2001 l`Inventari federal da las plazzas da fregar per amfibis cun 701 objects. Ils onns 2003, 2007, 2017 e 2025 è quel vegnì revedì. Actualmain èn en vigur 969 objects (873 objects fixs e 96 objects movibels). Plinavant cuntegna l`agiunta 3 tut en tut 25 objects, dals quals ils perimeters n`èn betg anc rectifitgads definitivamain. Fin ch`igl è decidì d`als integrar en l`agiunta 1 u 2, sa drizza lur protecziun tenor l`artitgel 29 alinea 1 litera a da l`Ordinaziun davart la protecziun da la natira e da la patria (OPNP) e tenor l`artitgel 10 da l`Ordinaziun davart la protecziun da las plazzas da fregar per amfibis d`impurtanza naziunala (OPFA).</Abstract>
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        <Abstract>L`unitad da datas cuntegna bloccadas e sviaments sin las rutas da &#39;La Svizra cun velo da muntogna&#39; en Svizra ed en il Principadi da Liechtenstein, ch`èn vegnids communitgads a SvizraMobila. L`unitad da datas cumplettescha l`unitad da geodatas da basa &#39;La Svizra cun velo da muntogna&#39; (traffic betg motorisà - &#39;La Svizra cun velo da muntogna&#39;) e vegn publitgada da l`Uffizi federal da vias UVIAS, da l`Uffizi federal da topografia swisstopo, da SvizraMobila e dals chantuns. Link al disclaimer: https://www.schweizmobil.ch/de/unterseiten/disclaimer_de.html</Abstract>
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