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

D 2008

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

TESAŘ, Miroslav, Miroslav ŠÍR, Miroslav KREJČA a Jan VÁCHAL

Základní údaje

Originální název

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

Název česky

Vliv vegetačního krytu na teplotu vzduchu a půdy na Šumavě

Autoři

TESAŘ, Miroslav, Miroslav ŠÍR, Miroslav KREJČA a Jan VÁCHAL

Vydání

Ljubljana, Conference abstracts. XXIVth Conference of the Danubian Countries on the Hydrological Forecasting and Hydrological Bases of Water Management, 1 s. 2008

Nakladatel

Slovenian National Committee

Další údaje

Jazyk

angličtina

Typ výsledku

Stať ve sborníku

Obor

10000 1. Natural Sciences

Stát vydavatele

Česká republika

Utajení

není předmětem státního či obchodního tajemství

ISBN

978-961-91090-3-8

Klíčová slova anglicky

plant transpiration; climate; thermal regime

Návaznosti

SP/1A6/151/07, projekt VaV.

Změněno: 25. 8. 2010 10:43, Věra Kostková

Anotace

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. ...

Citovat

TESAŘ, Miroslav, Miroslav ŠÍR, Miroslav KREJČA a Jan VÁCHAL. Influence of vegetation cover on air and soil temperatures in the Šumava MTS. (Czech Republic). In Conference abstracts. XXIVth Conference of the Danubian Countries on the Hydrological Forecasting and Hydrological Bases of Water Management. Ljubljana: Slovenian National Committee, 2008, 1 s. ISBN 978-961-91090-3-8.

@inproceedings{11201,
   author = {Tesař, Miroslav and Šír, Miroslav and Krejča, Miroslav and Váchal, Jan},
   address = {Ljubljana},
   booktitle = {Conference abstracts. XXIVth Conference of the Danubian Countries on the Hydrological Forecasting and Hydrological Bases of Water Management},
   keywords = {plant transpiration; climate; thermal regime},
   language = {eng},
   location = {Ljubljana},
   isbn = {978-961-91090-3-8},
   publisher = {Slovenian National Committee},
   title = {Influence of vegetation cover on air and soil temperatures in the Šumava MTS. (Czech Republic)},
   year = {2008}
}

TY  - JOUR
ID  - 11201
AU  - Tesař, Miroslav - Šír, Miroslav - Krejča, Miroslav - Váchal, Jan
PY  - 2008
TI  - Influence of vegetation cover on air and soil temperatures in the Šumava MTS. (Czech Republic)
PB  - Slovenian National Committee
CY  - Ljubljana
SN  - 9789619109038
KW  - plant transpiration
KW  - climate
KW  - thermal regime
N2  - 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. ...
ER  -

TESAŘ, Miroslav, Miroslav ŠÍR, Miroslav KREJČA a Jan VÁCHAL. Influence of vegetation cover on air and soil temperatures in the Šumava MTS. (Czech Republic). In \textit{Conference abstracts. XXIVth Conference of the Danubian Countries on the Hydrological Forecasting and Hydrological Bases of Water Management}. Ljubljana: Slovenian National Committee, 2008, 1 s. ISBN~978-961-91090-3-8.

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