Climate model differences contribute deep uncertainty in future Antarctic ice loss

被引:11
|
作者
Li, Dawei [1 ,2 ,3 ,4 ]
DeConto, Robert M. [2 ]
Pollard, David [2 ,5 ]
机构
[1] Shanghai Jiao Tong Univ, Sch Oceanog, Shanghai 200030, Peoples R China
[2] Univ Massachusetts Amherst, Dept Geosci, Amherst, MA 01003 USA
[3] Polar Res Inst China, MNR Key Lab Polar Sci, Shanghai 200136, Peoples R China
[4] Shanghai Jiao Tong Univ, Shanghai Key Lab Polar Life & Environm Sci, Shanghai 200030, Peoples R China
[5] Penn State Univ, Earth & Environm Syst Inst, University Pk, PA 16802 USA
基金
美国国家科学基金会; 中国国家自然科学基金; 上海市自然科学基金;
关键词
SEA-LEVEL; CLIFF INSTABILITY; MASS-BALANCE; SHEET;
D O I
10.1126/sciadv.add7082
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Future projections of ice sheets in response to different climate scenarios and their associated contributions to sea level changes are subject to deep uncertainty due to ice sheet instability processes, hampering a proper risk assessment of sea level rise and enaction of mitigation/adaptation strategies. For a systematic evaluation of the uncertainty due to climate model fields used as input to the ice sheet models, we drive a three-dimensional model of the Antarctic Ice Sheet (AIS) with the output from 36 climate models to simulate past and future changes in the AIS. Simulations show that a few climate models result in partial collapse of the West AIS under modeled preindustrial climates, and the spread in future changes in the AIS's volume is comparable to the structural uncertainty originating from differing ice sheet models. These results highlight the need for im-proved representations of physical processes important for polar climate in climate models.
引用
收藏
页数:15
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