Soil water movement during extreme precipitation in the Šumava Mts. and the Krkonoše Mts. in August 2002

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985874%3A_____%2F10%3A00341782" target="_blank" >RIV/67985874:_____/10:00341782 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/68378289:_____/10:00341782

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Soil water movement during extreme precipitation in the Šumava Mts. and the Krkonoše Mts. in August 2002

Popis výsledku v původním jazyce

The paper looks at soil water movement during extreme rainfall events in the Doupě and Kout catchments (Šumava Mts.) as well as the Modrý Důl catchment (Krkonoše Mts.). Two cyclones, which moved from Hungary to Poland, caused extreme rainfall and subsequent extreme runoff in August, 2002. Precipitation, air and soil temperature, and tensiometric pressure were recorded in each catchment. Analysis has shown that the immense amount of rainfall in August 2002 exceeded the retention capacity of the catchments covered by mature spruce forest and dwarf pine forest (Modrý Důl), dead forest and herb undergrowth (Kout), and a clearing covered by herbs (Doupě). This indicates that plant cover played a negligible role in runoff formation. The soil cover in the mountains, formed of Eutric Cambisols (Kout and Doupě) as well as Humic Podzols and Lithic Leptosols (Modrý Důl), was not able to prevent catastrophic runoff conditions because its retention capacity is rather low (60?90 mm).

Název v anglickém jazyce

Soil water movement during extreme precipitation in the Šumava Mts. and the Krkonoše Mts. in August 2002

Popis výsledku anglicky

The paper looks at soil water movement during extreme rainfall events in the Doupě and Kout catchments (Šumava Mts.) as well as the Modrý Důl catchment (Krkonoše Mts.). Two cyclones, which moved from Hungary to Poland, caused extreme rainfall and subsequent extreme runoff in August, 2002. Precipitation, air and soil temperature, and tensiometric pressure were recorded in each catchment. Analysis has shown that the immense amount of rainfall in August 2002 exceeded the retention capacity of the catchments covered by mature spruce forest and dwarf pine forest (Modrý Důl), dead forest and herb undergrowth (Kout), and a clearing covered by herbs (Doupě). This indicates that plant cover played a negligible role in runoff formation. The soil cover in the mountains, formed of Eutric Cambisols (Kout and Doupě) as well as Humic Podzols and Lithic Leptosols (Modrý Důl), was not able to prevent catastrophic runoff conditions because its retention capacity is rather low (60?90 mm).

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2010

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Folia Geographica

ISSN

0071-6715

e-ISSN

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Svazek periodika

41

Číslo periodika v rámci svazku

-

Stát vydavatele periodika

PL - Polská republika

Počet stran výsledku

7

Strana od-do

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Kód UT WoS článku

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EID výsledku v databázi Scopus

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