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Statements

Subject Item
n2:RIV%2F67985530%3A_____%2F12%3A00381318%21RIV13-AV0-67985530
rdf:type
n9:Vysledek skos:Concept
dcterms:description
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. 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.
dcterms:title
Western Canadian Sedimentary Basin temperature–depth transients from repeated well logs: evidence of recent decade subsurface heat gain due to climatic warming Western Canadian Sedimentary Basin temperature–depth transients from repeated well logs: evidence of recent decade subsurface heat gain due to climatic warming
skos:prefLabel
Western Canadian Sedimentary Basin temperature–depth transients from repeated well logs: evidence of recent decade subsurface heat gain due to climatic warming Western Canadian Sedimentary Basin temperature–depth transients from repeated well logs: evidence of recent decade subsurface heat gain due to climatic warming
skos:notation
RIV/67985530:_____/12:00381318!RIV13-AV0-67985530
n9:predkladatel
n10:ico%3A67985530
n4:aktivita
n19:Z
n4:aktivity
Z(AV0Z30120515)
n4:cisloPeriodika
2
n4:dodaniDat
n17:2013
n4:domaciTvurceVysledku
n11:6715125
n4:druhVysledku
n8:J
n4:duvernostUdaju
n5:S
n4:entitaPredkladatele
n14:predkladatel
n4:idSjednocenehoVysledku
180854
n4:idVysledku
RIV/67985530:_____/12:00381318
n4:jazykVysledku
n15:eng
n4:klicovaSlova
borehole temperatures; climate warming; ground heat flux and heat gain; Canadian Prairies
n4:klicoveSlovo
n6:Canadian%20Prairies n6:ground%20heat%20flux%20and%20heat%20gain n6:climate%20warming n6:borehole%20temperatures
n4:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n4:kontrolniKodProRIV
[73977C2AED33]
n4:nazevZdroje
Journal of Geophysics and Engineering
n4:obor
n18:DC
n4:pocetDomacichTvurcuVysledku
1
n4:pocetTvurcuVysledku
3
n4:rokUplatneniVysledku
n17:2012
n4:svazekPeriodika
9
n4:tvurceVysledku
Majorowicz, J. Skinner, W. Šafanda, Jan
n4:wos
000302142200002
n4:zamer
n12:AV0Z30120515
s:issn
1742-2132
s:numberOfPages
11
n3:doi
10.1088/1742-2132/9/2/127