Six years of ground?air temperature tracking at Malence (Slovenia): thermal diffusivity from subsurface temperature data

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F13%3A00396855" target="_blank" >RIV/67985530:_____/13:00396855 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1088/1742-2132/10/2/025012" target="_blank" >http://dx.doi.org/10.1088/1742-2132/10/2/025012</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1088/1742-2132/10/2/025012" target="_blank" >10.1088/1742-2132/10/2/025012</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Six years of ground?air temperature tracking at Malence (Slovenia): thermal diffusivity from subsurface temperature data

Popis výsledku v původním jazyce

To understand the processes which govern the downward propagation of the surface temperature signal and to quantify the relationship between ground and air temperatures, a borehole climate observatory was established at Malence (Slovenia). A substantial(climate?) warming has been observed; surface air temperature from 2003 to 2009 has been increasing by a rate of more than 0.5 K/year. Temperature difference between ground and air temperatures revealed a typical annual course; during the winter months the ground is warmer than the air, in the summer the ground gets slightly colder, the mean yearly offset value amounting to 1.6 K. Here we report on the thermal diffusivity distribution which was determined for a near-surface 10 m deep section using a number of six-year-long temperature?time data series.

Název v anglickém jazyce

Six years of ground?air temperature tracking at Malence (Slovenia): thermal diffusivity from subsurface temperature data

Popis výsledku anglicky

To understand the processes which govern the downward propagation of the surface temperature signal and to quantify the relationship between ground and air temperatures, a borehole climate observatory was established at Malence (Slovenia). A substantial(climate?) warming has been observed; surface air temperature from 2003 to 2009 has been increasing by a rate of more than 0.5 K/year. Temperature difference between ground and air temperatures revealed a typical annual course; during the winter months the ground is warmer than the air, in the summer the ground gets slightly colder, the mean yearly offset value amounting to 1.6 K. Here we report on the thermal diffusivity distribution which was determined for a near-surface 10 m deep section using a number of six-year-long temperature?time data series.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DC - Seismologie, vulkanologie a struktura Země

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název periodika

Journal of Geophysics and Engineering

ISSN

1742-2132

e-ISSN

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Svazek periodika

10

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

9

Strana od-do

"025012/1"-"025012/9"

Kód UT WoS článku

000317336400012

EID výsledku v databázi Scopus

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