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rdf:type
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Description
| - The role of water movement and retention during extreme runoff formation was demonstrated in the Modrý Důl catchment (Krkonoše Mts., Czech Republic). A cyclone, which moved from Hungary to Poland, caused extreme rain (120 mm) and subsequent extreme runoff in August, 2002. Precipitation, discharge, air and soil temperature, tensiometric pressure, and soil moisture were recorded. The maximum retention capacity of the catchment was evaluated (70 mm). Depending on actual retention capacity and precipitation amount two situations were recorded: (1) Precipitation amount less than actual retention capacity where precipitation was fully absorbed in the catchment and the discharge in the stream was not influenced by rain. (2) Precipitation amount greater than actual retention capacity where precipitation caused a saturation excess of the soil profile, generating extreme outflow in the stream.
- The role of water movement and retention during extreme runoff formation was demonstrated in the Modrý Důl catchment (Krkonoše Mts., Czech Republic). A cyclone, which moved from Hungary to Poland, caused extreme rain (120 mm) and subsequent extreme runoff in August, 2002. Precipitation, discharge, air and soil temperature, tensiometric pressure, and soil moisture were recorded. The maximum retention capacity of the catchment was evaluated (70 mm). Depending on actual retention capacity and precipitation amount two situations were recorded: (1) Precipitation amount less than actual retention capacity where precipitation was fully absorbed in the catchment and the discharge in the stream was not influenced by rain. (2) Precipitation amount greater than actual retention capacity where precipitation caused a saturation excess of the soil profile, generating extreme outflow in the stream. (en)
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Title
| - Extreme runoff formation in the Krkonoše Mts. in August 2002
- Extreme runoff formation in the Krkonoše Mts. in August 2002 (en)
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skos:prefLabel
| - Extreme runoff formation in the Krkonoše Mts. in August 2002
- Extreme runoff formation in the Krkonoše Mts. in August 2002 (en)
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skos:notation
| - RIV/68378289:_____/08:00341883!RIV10-MZP-68378289
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http://linked.open...avai/riv/aktivita
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http://linked.open...avai/riv/aktivity
| - P(1QS200420562), P(GA205/05/2312), P(GA205/06/0375), P(SP/1A6/151/07), Z(AV0Z20600510), Z(AV0Z30420517)
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http://linked.open...iv/cisloPeriodika
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http://linked.open...vai/riv/dodaniDat
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http://linked.open...aciTvurceVysledku
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http://linked.open.../riv/druhVysledku
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http://linked.open...iv/duvernostUdaju
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http://linked.open...titaPredkladatele
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http://linked.open...dnocenehoVysledku
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http://linked.open...ai/riv/idVysledku
| - RIV/68378289:_____/08:00341883
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http://linked.open...riv/jazykVysledku
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http://linked.open.../riv/klicovaSlova
| - hydrologic cycle; evapotranspiration; gross primary productivity; entropy production; soil water retention (en)
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http://linked.open.../riv/klicoveSlovo
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http://linked.open...odStatuVydavatele
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http://linked.open...ontrolniKodProRIV
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http://linked.open...i/riv/nazevZdroje
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http://linked.open...in/vavai/riv/obor
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http://linked.open...ichTvurcuVysledku
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http://linked.open...cetTvurcuVysledku
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http://linked.open...vavai/riv/projekt
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http://linked.open...UplatneniVysledku
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http://linked.open...v/svazekPeriodika
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http://linked.open...iv/tvurceVysledku
| - Tesař, Miroslav
- Šír, Miloslav
- Lichner, Ľ.
- Fišák, Jaroslav
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http://linked.open...n/vavai/riv/zamer
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issn
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number of pages
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