Evaluation of soil temperature in long-term series

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43210%2F17%3A43912937" target="_blank" >RIV/62156489:43210/17:43912937 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00020699:_____/17:N0000104

Výsledek na webu

<a href="http://sbks.sk/smolenice/Hajkova%20et%20al%20temperature.pdf" target="_blank" >http://sbks.sk/smolenice/Hajkova%20et%20al%20temperature.pdf</a>

DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Evaluation of soil temperature in long-term series

Popis výsledku v původním jazyce

Soil is an essential component of the environment - it makes the main conditions for life on the Earth. It plays an important role in the stability of ecosystems by influence of balance of matter and energy and in the hydrological cycle. That&apos;s why physical properties of the soil have a significant role in many processes, especially in the chemical and biological interactions which are bound to the soil environment. The most important is the conversion of solar radiation into heat and the subsequent distribution of energy flows. All these processes depend on the content of soil water, air and also on soil temperature. The soil temperature is measured at stations of the Czech Hydrometeorological Institute at depths of 5, 10, 20, 50 and 100 cm under grassland. In this paper were analyzed daily values of soil temperature at depth of 5, 10, 20, 50 and 100 cm within period 1961-2016 from selected CHMI stations at different altitudes using statictical software. Soil temperature was also evaluated in dependence on snow cover.

Název v anglickém jazyce

Evaluation of soil temperature in long-term series

Popis výsledku anglicky

Soil is an essential component of the environment - it makes the main conditions for life on the Earth. It plays an important role in the stability of ecosystems by influence of balance of matter and energy and in the hydrological cycle. That&apos;s why physical properties of the soil have a significant role in many processes, especially in the chemical and biological interactions which are bound to the soil environment. The most important is the conversion of solar radiation into heat and the subsequent distribution of energy flows. All these processes depend on the content of soil water, air and also on soil temperature. The soil temperature is measured at stations of the Czech Hydrometeorological Institute at depths of 5, 10, 20, 50 and 100 cm under grassland. In this paper were analyzed daily values of soil temperature at depth of 5, 10, 20, 50 and 100 cm within period 1961-2016 from selected CHMI stations at different altitudes using statictical software. Soil temperature was also evaluated in dependence on snow cover.

Druh

D - Stať ve sborníku

CEP obor

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OECD FORD obor

10510 - Climatic research

Projekt

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Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2017

Kód důvěrnosti údajů

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

Název statě ve sborníku

Snow an ecological phenomenon: Conference proceedings

ISBN

978-80-89703-47-0

ISSN

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e-ISSN

neuvedeno

Počet stran výsledku

3

Strana od-do

&quot;Nestrankovano&quot;

Název nakladatele

Slovenská botanická spoločnosť pri SAV

Místo vydání

Bratislava

Místo konání akce

Smolenice

Datum konání akce

19. 9. 2017

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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