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Statements

Subject Item
n2:RIV%2F67985530%3A_____%2F14%3A00433129%21RIV15-AV0-67985530
rdf:type
skos:Concept n13:Vysledek
dcterms:description
The %22low%22 in the transient temperature versus depth borehole profiles around 120 m seen from deep temperature logs in the Canadian Prairies (southern Alberta-southern Saskatchewan), as well as in some of the European data, has been interpreted to be related to the Little Ice Age (LIA). Data point to the lowest ground surface and subsurface temperatures occurring in the very late eighteenth to nineteenth centuries. Inversion of these logs shows that surface temperature lows were followed by a recent warming period. Further, the synthetic profiles built on the basis of solar forcing history, stretching as far back as the beginning of the seventeenth century, suggest that the LIA signatures interpreted from the inversion of the borehole temperature logs would be difficult to be explained by known published models of past solar irradiation despite large range of assumed sensitivities for the couplings assumed, and that further forcing needs to be considered. The %22low%22 in the transient temperature versus depth borehole profiles around 120 m seen from deep temperature logs in the Canadian Prairies (southern Alberta-southern Saskatchewan), as well as in some of the European data, has been interpreted to be related to the Little Ice Age (LIA). Data point to the lowest ground surface and subsurface temperatures occurring in the very late eighteenth to nineteenth centuries. Inversion of these logs shows that surface temperature lows were followed by a recent warming period. Further, the synthetic profiles built on the basis of solar forcing history, stretching as far back as the beginning of the seventeenth century, suggest that the LIA signatures interpreted from the inversion of the borehole temperature logs would be difficult to be explained by known published models of past solar irradiation despite large range of assumed sensitivities for the couplings assumed, and that further forcing needs to be considered.
dcterms:title
The Little Ice Age signature and subsequent warming seen in borehole temperature logs versus solar forcing model The Little Ice Age signature and subsequent warming seen in borehole temperature logs versus solar forcing model
skos:prefLabel
The Little Ice Age signature and subsequent warming seen in borehole temperature logs versus solar forcing model The Little Ice Age signature and subsequent warming seen in borehole temperature logs versus solar forcing model
skos:notation
RIV/67985530:_____/14:00433129!RIV15-AV0-67985530
n3:aktivita
n8:I
n3:aktivity
I
n3:cisloPeriodika
4
n3:dodaniDat
n9:2015
n3:domaciTvurceVysledku
n7:6715125
n3:druhVysledku
n10:J
n3:duvernostUdaju
n12:S
n3:entitaPredkladatele
n16:predkladatel
n3:idSjednocenehoVysledku
26399
n3:idVysledku
RIV/67985530:_____/14:00433129
n3:jazykVysledku
n15:eng
n3:klicovaSlova
surface processes; borehole temperatures; climatic warming; Little Ice Age; solar irradiation
n3:klicoveSlovo
n4:Little%20Ice%20Age n4:solar%20irradiation n4:climatic%20warming n4:borehole%20temperatures n4:surface%20processes
n3:kodStatuVydavatele
DE - Spolková republika Německo
n3:kontrolniKodProRIV
[1F1D6001322B]
n3:nazevZdroje
International Journal of Earth Sciences
n3:obor
n17:DC
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
3
n3:rokUplatneniVysledku
n9:2014
n3:svazekPeriodika
103
n3:tvurceVysledku
Šafanda, Jan Przybylak, R. Majorowicz, J.
n3:wos
000335957200012
s:issn
1437-3254
s:numberOfPages
11
n11:doi
10.1007/s00531-014-1008-7