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Midlatitude land surface temperature impactsthe timing and structure of glacial maxima
Thomas,E.K(Thomas,Elizabeth K)1,2; Clemens,S.C(Clemens,Steven C)1; Sun,YB(Sun,Youbin)3; Huang,YS(Huang,Yongsong)1; Prell,W(Prell,Warren)1; Chen,GS(Chen,Guangshan)4; Liu,ZY(Liu,Zhengyu)4; Loomis,S(Loomis,Shannon)5; Thomas,Elizabeth K
2017-01-10
发表期刊Geophysical Research Letters
卷号44期号:2017页码:984-992
文章类型期刊论文
摘要Orbitally modulated insolation is thought to be among the key mechanisms driving ice sheet change. Yet, late Pleistocene ice sheets attained maximum marginal extents prior to summer insolation minima, suggesting that additional mechanisms influenced ice growth and decay. Continuous orbital‐scale terrestrial temperature records can help define the role that temperature near ice sheet margins plays on the timing and structure of glacial maxima. We hypothesize, based on a 360 kyr long air temperature record from the Chinese Loess Plateau and shorter records from North America and Europe, that midlatitude terrestrial temperature influenced the rate of ice sheet growth prior to and during glacial maxima; cold conditions prior to glacial maxima enhanced ice sheet growth, while warming during glacial maxima inhibited further growth, despite low summer insolation. Thus, the midlatitude surface energy budget may be an important component of understanding and modeling ice volume, particularly for intervals prior to and during glacial maxima, when ice sheet margins reached midlatitudes.
DOI10.1002/2016GL071882
收录类别SCI
所属项目编号KZZD-EW-TZ-03
语种英语
项目资助者NSFGraduate Research Fellowship to E.K.T.,NSF AGS-1002504 and OCE-1129408 toS.C.C. ; NSFGraduate Research Fellowship to E.K.T.,NSF AGS-1002504 and OCE-1129408 toS.C.C. ; International InnovationPartnership Program from the ChineseAcademy of Sciences to Y.S., NSF 1129316 to G.C., and NSF41130105 to Z.L ; International InnovationPartnership Program from the ChineseAcademy of Sciences to Y.S., NSF 1129316 to G.C., and NSF41130105 to Z.L
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被引频次:2[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.ieecas.cn/handle/361006/5606
专题古环境研究室
通讯作者Thomas,Elizabeth K
作者单位1.Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, Rhode Island, USA
2.Now atDepartment of Geology, University at Buffalo, Buffalo, New York, USA
3.Laboratory for Loess and Quaternary Geology,Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China
4.Department of Atmospheric and OceanSciences, University of Wisconsin-Madison, Madison, Wisconsin, USA
5.Jackson School of Geosciences, University of Texas atAustin, Austin, Texas, USA
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Thomas,E.K,Clemens,S.C,Sun,YB,et al. Midlatitude land surface temperature impactsthe timing and structure of glacial maxima[J]. Geophysical Research Letters,2017,44(2017):984-992.
APA Thomas,E.K.,Clemens,S.C.,Sun,YB.,Huang,YS.,Prell,W.,...&Thomas,Elizabeth K.(2017).Midlatitude land surface temperature impactsthe timing and structure of glacial maxima.Geophysical Research Letters,44(2017),984-992.
MLA Thomas,E.K,et al."Midlatitude land surface temperature impactsthe timing and structure of glacial maxima".Geophysical Research Letters 44.2017(2017):984-992.
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