中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Modeling a modern-like pCO(2) warm period (Marine Isotope Stage KM5c) with two versions of an Institut Pierre Simon Laplace atmosphere-ocean coupled general circulation model

文献类型:期刊论文

作者Tan, Ning2,3; Contoux, Camille3; Ramstein, Gilles3; Sun, Yong1; Dumas, Christophe3; Sepulchre, Pierre3; Guo, Zhengtang2,4
刊名CLIMATE OF THE PAST
出版日期2020-01-06
卷号16期号:1页码:1-16
ISSN号1814-9324
DOI10.5194/cp-16-1-2020
英文摘要The mid-Piacenzian warm period (3.264 to 3.025 Ma) is the most recent geological period with present-like atmospheric pCO(2) and is thus expected to have exhibited a warm climate similar to or warmer than the present day. On the basis of understanding that has been gathered on the climate variability of this interval, a specific interglacial (Marine Isotope Stage KM5c, MIS KM5c; 3.205 Ma) has been selected for the Pliocene Model Intercomparison Project phase 2 (PlioMIP 2). We carried out a series of experiments according to the design of PlioMIP2 with two versions of the Institut Pierre Simon Laplace (IPSL) atmosphere-ocean coupled general circulation model (AOGCM): IPSL-CM5A and IPSL-CM5A2. Compared to the PlioMIP 1 experiment, run with IPSL-CM5A, our results show that the simulated MIS KM5c climate presents enhanced warming in mid- to high latitudes, especially over oceanic regions. This warming can be largely attributed to the enhanced Atlantic Meridional Overturning Circulation caused by the high-latitude seaway changes. The sensitivity experiments, conducted with IPSL-CM5A2, show that besides the increased pCO(2), both modified orography and reduced ice sheets contribute substantially to mid- to high latitude warming in MIS KM5c. When considering the pCO(2) uncertainties (+/-50 ppmv) during the Pliocene, the response of the modeled mean annual surface air temperature to changes to pCO(2) (+/-50 ppmv) is not symmetric, which is likely due to the nonlinear response of the cryosphere (snow cover and sea ice extent). By analyzing the Greenland Ice Sheet surface mass balance, we also demonstrate its vulnerability under both MIS KM5c and modern warm climate.
WOS关键词GREENLAND ICE-SHEET ; MERIDIONAL OVERTURNING CIRCULATION ; MID-PLIOCENE ; SEA-ICE ; SURFACE TEMPERATURES ; CLIMATE SIMULATIONS ; GLOBAL CLIMATE ; VEGETATION ; SENSITIVITY ; AMPLIFICATION
资助项目French State Program Investissements d'Avenir ; ANR HADOC project[ANR-17-CE31-0010] ; Basic Science Center Project of the National Science Foundation of China[41888101] ; Strategic Priority Research Program[XDB 26000000]
WOS研究方向Geology ; Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000505954800001
出版者COPERNICUS GESELLSCHAFT MBH
资助机构French State Program Investissements d'Avenir ; French State Program Investissements d'Avenir ; French State Program Investissements d'Avenir ; French State Program Investissements d'Avenir ; ANR HADOC project ; ANR HADOC project ; ANR HADOC project ; ANR HADOC project ; Basic Science Center Project of the National Science Foundation of China ; Basic Science Center Project of the National Science Foundation of China ; Basic Science Center Project of the National Science Foundation of China ; Basic Science Center Project of the National Science Foundation of China ; Strategic Priority Research Program ; Strategic Priority Research Program ; Strategic Priority Research Program ; Strategic Priority Research Program ; French State Program Investissements d'Avenir ; French State Program Investissements d'Avenir ; French State Program Investissements d'Avenir ; French State Program Investissements d'Avenir ; ANR HADOC project ; ANR HADOC project ; ANR HADOC project ; ANR HADOC project ; Basic Science Center Project of the National Science Foundation of China ; Basic Science Center Project of the National Science Foundation of China ; Basic Science Center Project of the National Science Foundation of China ; Basic Science Center Project of the National Science Foundation of China ; Strategic Priority Research Program ; Strategic Priority Research Program ; Strategic Priority Research Program ; Strategic Priority Research Program ; French State Program Investissements d'Avenir ; French State Program Investissements d'Avenir ; French State Program Investissements d'Avenir ; French State Program Investissements d'Avenir ; ANR HADOC project ; ANR HADOC project ; ANR HADOC project ; ANR HADOC project ; Basic Science Center Project of the National Science Foundation of China ; Basic Science Center Project of the National Science Foundation of China ; Basic Science Center Project of the National Science Foundation of China ; Basic Science Center Project of the National Science Foundation of China ; Strategic Priority Research Program ; Strategic Priority Research Program ; Strategic Priority Research Program ; Strategic Priority Research Program ; French State Program Investissements d'Avenir ; French State Program Investissements d'Avenir ; French State Program Investissements d'Avenir ; French State Program Investissements d'Avenir ; ANR HADOC project ; ANR HADOC project ; ANR HADOC project ; ANR HADOC project ; Basic Science Center Project of the National Science Foundation of China ; Basic Science Center Project of the National Science Foundation of China ; Basic Science Center Project of the National Science Foundation of China ; Basic Science Center Project of the National Science Foundation of China ; Strategic Priority Research Program ; Strategic Priority Research Program ; Strategic Priority Research Program ; Strategic Priority Research Program
源URL[http://ir.iggcas.ac.cn/handle/132A11/95864]  
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Tan, Ning
作者单位1.Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modelling Atmospher Sci & Geo, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
3.Univ Paris Saclay, CEA, LSCE, CNRS,UVSQ,IPSL, F-91191 Gif Sur Yvette, France
4.Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China
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Tan, Ning,Contoux, Camille,Ramstein, Gilles,et al. Modeling a modern-like pCO(2) warm period (Marine Isotope Stage KM5c) with two versions of an Institut Pierre Simon Laplace atmosphere-ocean coupled general circulation model[J]. CLIMATE OF THE PAST,2020,16(1):1-16.
APA Tan, Ning.,Contoux, Camille.,Ramstein, Gilles.,Sun, Yong.,Dumas, Christophe.,...&Guo, Zhengtang.(2020).Modeling a modern-like pCO(2) warm period (Marine Isotope Stage KM5c) with two versions of an Institut Pierre Simon Laplace atmosphere-ocean coupled general circulation model.CLIMATE OF THE PAST,16(1),1-16.
MLA Tan, Ning,et al."Modeling a modern-like pCO(2) warm period (Marine Isotope Stage KM5c) with two versions of an Institut Pierre Simon Laplace atmosphere-ocean coupled general circulation model".CLIMATE OF THE PAST 16.1(2020):1-16.

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来源:地质与地球物理研究所

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