Extrémní povodně v Krkonoších

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F08%3A00319203" target="_blank" >RIV/68378289:_____/08:00319203 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985874:_____/08:00319203

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Extreme floods in the Krkonoše Mts. (Czech Republic) in summer 2002 and 2006

Popis výsledku v původním jazyce

Hydrological and meteorological conditions preceding two extreme periods of rainfall in the Krkonoše Mts. in summer 2002 and 2006 are discussed. Heavy rains in August 2002 and 2006 were caused by cyclones of Mediterranean origin. We analyze the role of insufficient plant transpiration in the formation of the two events. Meteorological data demonstrate that air temperatures were high for many days before the extreme rainfall in the Central Europe including the Krkonoše Mts. This indicates the possibilitythat overheating of the air was caused by insufficient precipitation, resulting in the lack of transpiration cooling of the Krkonoše Mts. In contrast, high soil moisture recorded in the Krkonoše Mts. before the extreme rainfall provides evidence that plant transpiration in the Krkonoše Mts. was not limited by water shortage. This means that the source of air overheating was outside the Krkonoše Mts.

Název v anglickém jazyce

Extreme floods in the Krkonoše Mts. (Czech Republic) in summer 2002 and 2006

Popis výsledku anglicky

Hydrological and meteorological conditions preceding two extreme periods of rainfall in the Krkonoše Mts. in summer 2002 and 2006 are discussed. Heavy rains in August 2002 and 2006 were caused by cyclones of Mediterranean origin. We analyze the role of insufficient plant transpiration in the formation of the two events. Meteorological data demonstrate that air temperatures were high for many days before the extreme rainfall in the Central Europe including the Krkonoše Mts. This indicates the possibilitythat overheating of the air was caused by insufficient precipitation, resulting in the lack of transpiration cooling of the Krkonoše Mts. In contrast, high soil moisture recorded in the Krkonoše Mts. before the extreme rainfall provides evidence that plant transpiration in the Krkonoše Mts. was not limited by water shortage. This means that the source of air overheating was outside the Krkonoše Mts.

Druh

D - Stať ve sborníku

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

<a href="/cs/project/1QS200420562" target="_blank" >1QS200420562: Měření množství usazených srážek a odhad mokré depozice polutantů</a><br>

Návaznosti

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

Rok uplatnění

2008

Kód důvěrnosti údajů

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

Název statě ve sborníku

24. Conference of the Danubian Countries on the Hydrological Forecasting and Hydrological Bases of Water Management

ISBN

978-961-91090-2-1

ISSN

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e-ISSN

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Počet stran výsledku

6

Strana od-do

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Název nakladatele

Slovenian National Committee for the IHP Unesco

Místo vydání

Ljubljana

Místo konání akce

Bled

Datum konání akce

2. 6. 2008

Typ akce podle státní příslušnosti

EUR - Evropská akce

Kód UT WoS článku

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