D
2008
Influence of vegetation cover on air and soil temperatures in the Šumava MTS. (Czech Republic)
TESAŘ, Miroslav, Miroslav ŠÍR, Miroslav KREJČA and Jan VÁCHAL
Basic information
Original name
Influence of vegetation cover on air and soil temperatures in the Šumava MTS. (Czech Republic)
Name in Czech
Vliv vegetačního krytu na teplotu vzduchu a půdy na Šumavě
Authors
TESAŘ, Miroslav, Miroslav ŠÍR, Miroslav KREJČA and
Jan VÁCHAL
Edition
Ljubljana, Conference abstracts. XXIVth Conference of the Danubian Countries on the Hydrological Forecasting and Hydrological Bases of Water Management, 1 pp. 2008
Publisher
Slovenian National Committee
Other information
Type of outcome
Stať ve sborníku
Field of Study
10000 1. Natural Sciences
Country of publisher
Czech Republic
Confidentiality degree
není předmětem státního či obchodního tajemství
Keywords in English
plant transpiration; climate; thermal regime
Links
SP/1A6/151/07, research and development project.
V originále
Plant transpiration modifies climatic conditions at the land surface and in the soil during the vegetative season (Eagelson 1987, Pokorný 2001). In mountainous areas of Central Europe transpiration recycles about 50% of the rainwater during the vegetative season. Evaporative cooling induced by transpiration reduces the maximum plant surface temperature by about 15C on a hot and dry day.Dissipation of solar energy in a landscape controlled by plant transpiration is the core of the terrestrial hydrologic cycle. Transpiration is substantially influenced by the form and functioning of the vegetation cover. ...
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