Assessing the stability of the Atlantic meridional overturning circulation of the past, present, and future

被引:9
作者
Liu Wei [1 ]
Liu Zhengyu [2 ,3 ]
机构
[1] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA
[2] Peking Univ, Lab Climate Ocean & Atmospher Studies, Beijing 100081, Peoples R China
[3] Univ Wisconsin, Ctr Climat Res, Madison, WI 53706 USA
基金
中国国家自然科学基金;
关键词
AMOC; stability indicator; freshwater transports; ITCZ; deglaciation; MULTIPLE EQUILIBRIA REGIME; MELTWATER PULSE 1A; THERMOHALINE CIRCULATION; ICE-SHEET; OCEAN CIRCULATION; DEEP CIRCULATION; AGULHAS LEAKAGE; SOUTH-ATLANTIC; CLIMATE-CHANGE; RAPID CHANGES;
D O I
10.1007/s13351-014-4006-6
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This paper is a review of the recent development of researches on the stability of the Atlantic meridional overturning circulation (AMOC). In particular, we will review recent studies that attempt to best assess the stability of the AMOC in the past, present, and future by using a stability indicator related to the freshwater transport by the AMOC. These studies further illustrate a potentially systematic bias in the state-of-the-art atmosphere-ocean general circulation models (AOGCMs), in which the AMOCs seem to be over-stabilized relative to that in the real world. This common model bias in the AMOC stability is contributed, partly, to a common tropical bias associated with the double intertropical convergence zone (ITCZ) in most state-of-the-art AOGCMs, casting doubts on future projection of abrupt climate changes in these climate models.
引用
收藏
页码:803 / 819
页数:17
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