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%2F67985874%3A_____%2F08%3A00319215" target="_blank" >RIV/67985874:_____/08:00319215 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985874:_____/08:00341878

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

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

2008

Kód důvěrnosti údajů

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

Název periodika

IOP Conference Series

ISSN

1755-1315

e-ISSN

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Svazek periodika

4

Číslo periodika v rámci svazku

-

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

8

Strana od-do

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Kód UT WoS článku

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EID výsledku v databázi Scopus

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