Vliv vegetačního krytu na teplotu vzduchu a půdy na Śumavě

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F75081431%3A_____%2F08%3A00000095" target="_blank" >RIV/75081431:_____/08:00000095 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Influence of vegetation cover on air and soil temperatures in the Šumava Mts. (Czech Republic)

Popis výsledku v původním jazyce

Air and soil temperature were measured in the cold climatic zone at three localities (catchments) under different plant cover during the growing seasons 2002-2007. The catchments Kout (dead forest), Doupě (clearing) and Stolec (mature spruce forest) aresituated in the National Park of the Šumava Mts. (1105-1330 m a. s. l.). The three catchments have very similar natural conditions, but differ significantly in vegetation cover. The following conclusions were obtained from the interpretation of measureddata: (1) The air temperature of the catchment covered by the dead forest had a greater daily fluctuation compared to the stands covered by clearing or mature forest. (2) The air temperature of catchments covered by mature forest had the smallest daily fluctuations. (3) The more extreme air temperatures in the dead forest caused the systematic raising of the soil temperature at a depth of 15 cm compared to soil in the clearing and mature forest.

Název v anglickém jazyce

Influence of vegetation cover on air and soil temperatures in the Šumava Mts. (Czech Republic)

Popis výsledku anglicky

Air and soil temperature were measured in the cold climatic zone at three localities (catchments) under different plant cover during the growing seasons 2002-2007. The catchments Kout (dead forest), Doupě (clearing) and Stolec (mature spruce forest) aresituated in the National Park of the Šumava Mts. (1105-1330 m a. s. l.). The three catchments have very similar natural conditions, but differ significantly in vegetation cover. The following conclusions were obtained from the interpretation of measureddata: (1) The air temperature of the catchment covered by the dead forest had a greater daily fluctuation compared to the stands covered by clearing or mature forest. (2) The air temperature of catchments covered by mature forest had the smallest daily fluctuations. (3) The more extreme air temperatures in the dead forest caused the systematic raising of the soil temperature at a depth of 15 cm compared to soil in the clearing and mature forest.

Druh

D - Stať ve sborníku

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)

Rok uplatnění

2008

Kód důvěrnosti údajů

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

Název statě ve sborníku

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

ISBN

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ISSN

1755-1307

e-ISSN

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Počet stran výsledku

8

Strana od-do

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Název nakladatele

Slovenian National Committee for the IHP UNESCO

Místo vydání

Ljubljana

Místo konání akce

Bled, Slovenia

Datum konání akce

2. 6. 2008

Typ akce podle státní příslušnosti

EUR - Evropská akce

Kód UT WoS článku

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