中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Comparison of Arctic and Southern Ocean sea ice between the last nine interglacials and the future

文献类型:期刊论文

作者Wu, Zhipeng1,2,3; Yin, Qiuzhen2; Guo, Zhengtang1,3,4; Berger, Andre2
刊名CLIMATE DYNAMICS
出版日期2022-01-23
页码11
关键词Sea ice Interglacials Insolation Arctic Southern Ocean CO2 Paleoclimate modeling
ISSN号0930-7575
DOI10.1007/s00382-022-06140-4
英文摘要Understanding the sea ice variability and the mechanisms involved during warm periods of the Earth is essential for a better understanding of the sea ice changes at the present and in the future. Based on simulations with the model LOVECLIM, this study investigates the sea ice variations during the last nine interglacials and focuses on the inter-comparison between interglacials as well as their differences from the present and future. Our results show that the annual mean Arctic sea ice variation is primarily controlled by local summer insolation, while the annual mean Southern Ocean sea ice variation is more influenced by the CO2 concentration but the effect of local summer insolation can't be ignored. The lowest Arctic sea ice area results from the highest summer insolation at MIS-15, and the lowest Southern Ocean sea ice area at MIS-9 is explained by the highest CO2 concentration and moderate local summer insolation. As compared to the present, the last nine interglacials all have much less sea ice in the Arctic annually and seasonally due to high summer insolation. They also have much less Arctic sea ice in summer than the double CO2 experiment, which makes to some degree the interglacials possible analogues for the future in terms of the changes of sea ice. However, compared to the double CO2 experiment, the interglacials all have much more sea ice in the Southern Ocean due to their much lower CO2 concentration, which suggests the inappropriateness of considering the interglacials as analogues for the future in the Southern Ocean. Our results suggest that in the search for potential analogues of the present and future climate, the seasonal and regional climate variations should be considered.
WOS关键词EQUILIBRIUM CLIMATE SENSITIVITY ; HOLOCENE ; MODEL ; ATMOSPHERE ; INSOLATION ; EVOLUTION ; CIRCULATION ; HISTORY ; RECORD ; END
资助项目Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS)[MIS F.4529.18] ; National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[41690114] ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS)[2.5020.11]
WOS研究方向Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000745793600002
出版者SPRINGER
资助机构Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; Fonds de la Recherche Scientifique-FNRS (F.R.S.-FNRS) ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS)
源URL[http://ir.iggcas.ac.cn/handle/132A11/104009]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Wu, Zhipeng; Yin, Qiuzhen
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing, Peoples R China
2.Catholic Univ Louvain, Georges Lemaitre Ctr Earth & Climate Res, Earth & Life Inst, Louvain La Neuve, Belgium
3.Univ Chinese Acad Sci, Beijing, Peoples R China
4.CAS Ctr Excellence Life & Paleoenvironm, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Wu, Zhipeng,Yin, Qiuzhen,Guo, Zhengtang,et al. Comparison of Arctic and Southern Ocean sea ice between the last nine interglacials and the future[J]. CLIMATE DYNAMICS,2022:11.
APA Wu, Zhipeng,Yin, Qiuzhen,Guo, Zhengtang,&Berger, Andre.(2022).Comparison of Arctic and Southern Ocean sea ice between the last nine interglacials and the future.CLIMATE DYNAMICS,11.
MLA Wu, Zhipeng,et al."Comparison of Arctic and Southern Ocean sea ice between the last nine interglacials and the future".CLIMATE DYNAMICS (2022):11.

入库方式: OAI收割

来源:地质与地球物理研究所

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