Midlatitude land surface temperature impactsthe timing and structure of glacial maxima
Prell,W(Prell,Warren)2; Sun,YB(Sun,Youbin)1; Liu,ZY(Liu,Zhengyu)5; Loomis,S(Loomis,Shannon)3; Huang,YS(Huang,Yongsong)2; Thomas,Elizabeth K; Thomas,E.K(Thomas,Elizabeth K)2,4; Clemens,S.C(Clemens,Steven C)2; Chen,GS(Chen,Guangshan)5
刊名Geophysical Research Letters
2017-01-10
卷号44期号:2017页码:984-992
DOI10.1002/2016GL071882
文献子类期刊论文
英文摘要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.
项目编号KZZD-EW-TZ-03
语种英语
资助机构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
内容类型期刊论文
源URL[http://ir.ieecas.cn/handle/361006/5606]  
专题地球环境研究所_古环境研究室
通讯作者Thomas,Elizabeth K
作者单位1.Laboratory for Loess and Quaternary Geology,Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China
2.Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, Rhode Island, USA
3.Jackson School of Geosciences, University of Texas atAustin, Austin, Texas, USA
4.Now atDepartment of Geology, University at Buffalo, Buffalo, New York, USA
5.Department of Atmospheric and OceanSciences, University of Wisconsin-Madison, Madison, Wisconsin, USA
推荐引用方式
GB/T 7714
Prell,W,Sun,YB,Liu,ZY,et al. Midlatitude land surface temperature impactsthe timing and structure of glacial maxima[J]. Geophysical Research Letters,2017,44(2017):984-992.
APA Prell,W.,Sun,YB.,Liu,ZY.,Loomis,S.,Huang,YS.,...&Chen,GS.(2017).Midlatitude land surface temperature impactsthe timing and structure of glacial maxima.Geophysical Research Letters,44(2017),984-992.
MLA Prell,W,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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