Počet záznamů: 1

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

SYSNO ASEP	0341782
Druh ASEP	J - Článek v odborném periodiku
Zařazení RIV	J - Článek v odborném periodiku
Poddruh J	Ostatní články
Název	Soil water movement during extreme precipitation in the Šumava Mts. and the Krkonoše Mts. in August 2002
Tvůrce(i)	Tesař, Miroslav (UH-J)_{ORCID, SAI, RID} Šír, Miloslav (UH-J)_{ORCID, RID, SAI} Krejča, M. (CZ) Fišák, Jaroslav (UFA-U)_RID Polívka, Jiří (UH-J)
Celkový počet autorů	5
Zdroj.dok.	Folia Geographica, Series Geographica - Physica - ISSN 0071-6715 Roč. 41, - (2010), s. 67-73
Poč.str.	7 s.
Jazyk dok.	eng - angličtina
Země vyd.	PL - Polsko
Klíč. slova	mountain hydrology ; extreme rain ; soil water movement
Vědní obor RIV	DA - Hydrologie a limnologie
CEP	1QS200420562 GA AV ČR - Akademie věd
	GA205/06/0375 GA ČR - Grantová agentura ČR
	GA205/08/1174 GA ČR - Grantová agentura ČR
	GA526/08/1016 GA ČR - Grantová agentura ČR
	SP/1A6/151/07 GA MŽP - Ministerstvo životního prostředí
CEZ	AV0Z20600510 - UH-J (2005-2011)
	AV0Z30420517 - UFA-U, BC-A (2005-2011)
Anotace	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).
Pracoviště	Ústav pro hydrodynamiku
Kontakt	Soňa Hnilicová, hnilicova@ih.cas.cz, Tel.: 233 109 003
Rok sběru	2011

Počet záznamů: 1