Western Canadian Sedimentary Basin temperature?depth transients from repeated well logs: evidence of recent decade subsurface heat gain due to climatic warming

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F12%3A00381318" target="_blank" >RIV/67985530:_____/12:00381318 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1088/1742-2132/9/2/127" target="_blank" >http://dx.doi.org/10.1088/1742-2132/9/2/127</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1088/1742-2132/9/2/127" target="_blank" >10.1088/1742-2132/9/2/127</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Western Canadian Sedimentary Basin temperature?depth transients from repeated well logs: evidence of recent decade subsurface heat gain due to climatic warming

Popis výsledku v původním jazyce

Temperature versus depth measurements in boreholes on the Canadian Prairies were originally measured some two decades ago (1987). They were repeated a decade ago and were then repeated from 2005 to 2007. Modelling of the synthetic temperature?depth transients shows that the time variation of subsurface temperature follows variations in surface air temperature (SAT). The surface-temperature increases of 0.2 and 0.4 °C are observed for time scales of one and two decades, respectively. The top of the atmosphere solar irradiance data recorded by satellite since 1978 was computed at the locations of the repeated temperature measurements to calculate a forcing signal to allow subsurface temperatures to be modelled, as previously done with SAT data.

Název v anglickém jazyce

Western Canadian Sedimentary Basin temperature?depth transients from repeated well logs: evidence of recent decade subsurface heat gain due to climatic warming

Popis výsledku anglicky

Temperature versus depth measurements in boreholes on the Canadian Prairies were originally measured some two decades ago (1987). They were repeated a decade ago and were then repeated from 2005 to 2007. Modelling of the synthetic temperature?depth transients shows that the time variation of subsurface temperature follows variations in surface air temperature (SAT). The surface-temperature increases of 0.2 and 0.4 °C are observed for time scales of one and two decades, respectively. The top of the atmosphere solar irradiance data recorded by satellite since 1978 was computed at the locations of the repeated temperature measurements to calculate a forcing signal to allow subsurface temperatures to be modelled, as previously done with SAT data.

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

—

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2012

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

—

Svazek periodika

9

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

11

Strana od-do

127-137

Kód UT WoS článku

000302142200002

EID výsledku v databázi Scopus

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