Key Laboratory for Virtual Geographic Environment, Ministry of
Education, State Key Laboratory Cultivation Base of Geographical Environment
Evolution of Jiangsu Province, Jiangsu Center for Collaborative Innovation
in Geographical Information Resource Development and Application, School of
Geography Science, Nanjing Normal University, Nanjing 210023, China
Department of Geology – Quaternary Science, Lund University, Lund,
223 62, Sweden
Key Laboratory for Virtual Geographic Environment, Ministry of
Education, State Key Laboratory Cultivation Base of Geographical Environment
Evolution of Jiangsu Province, Jiangsu Center for Collaborative Innovation
in Geographical Information Resource Development and Application, School of
Geography Science, Nanjing Normal University, Nanjing 210023, China
Jiangsu Provincial Key Laboratory for Numerical Simulation of
Large-Scale Complex Systems, School of Mathematical Science, Nanjing Normal
University, Nanjing 210023, China
Open Studio for the Simulation of Ocean-Climate-Isotope, Qingdao
National Laboratory for Marine Science and Technology, Qingdao 266237, China
Weiyi Sun
Key Laboratory for Virtual Geographic Environment, Ministry of
Education, State Key Laboratory Cultivation Base of Geographical Environment
Evolution of Jiangsu Province, Jiangsu Center for Collaborative Innovation
in Geographical Information Resource Development and Application, School of
Geography Science, Nanjing Normal University, Nanjing 210023, China
Lingfeng Wan
Institute of Advanced Ocean Study, Ocean University of China,
Qingdao, China
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Cumulative views and downloads
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Total article views: 1,917 (including HTML, PDF, and XML)
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1,330
500
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1,917
126
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Supplement: 126
BibTeX: 105
EndNote: 117
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Total article views: 2,940 (including HTML, PDF, and XML)
Thereof 2,781 with geography defined
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Total article views: 1,917 (including HTML, PDF, and XML)
Thereof 1,874 with geography defined
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Total article views: 1,023 (including HTML, PDF, and XML)
Thereof 907 with geography defined
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Based on proxy data and modeling, the Arctic temperature has an asymmetric cooling trend with more cooling over the Atlantic Arctic than the Pacific Arctic during the Holocene, dominated by orbital forcing. There is a seasonal difference in the asymmetric cooling trend, which is dominated by the DJF (December, January, and February) temperature variability. The Arctic dipole mode of sea level pressure and sea ice play a major role in asymmetric temperature changes.
Based on proxy data and modeling, the Arctic temperature has an asymmetric cooling trend with...
