Reducing spread in climate model projections of a September ice-free Arctic

被引:152
作者
Liu, Jiping [1 ]
Song, Mirong [2 ]
Horton, Radley M. [3 ]
Hu, Yongyun [4 ]
机构
[1] SUNY Albany, Dept Atmospher & Environm Sci, Albany, NY 12222 USA
[2] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China
[3] Columbia Univ, Ctr Climate Syst Res, New York, NY 10025 USA
[4] Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China
基金
中国国家自然科学基金; 美国国家航空航天局; 美国国家科学基金会;
关键词
SEA-ICE;
D O I
10.1073/pnas.1219716110
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
This paper addresses the specter of a September ice-free Arctic in the 21st century using newly available simulations from the Coupled Model Intercomparison Project Phase 5 (CMIP5). We find that large spread in the projected timing of the September ice-free Arctic in 30 CMIP5 models is associated at least as much with different atmospheric model components as with initial conditions. Here we reduce the spread in the timing of an ice-free state using two different approaches for the 30 CMIP5 models: (i) model selection based on the ability to reproduce the observed sea ice climatology and variability since 1979 and (ii) constrained estimation based on the strong and persistent relationship between present and future sea ice conditions. Results from the two approaches show good agreement. Under a high-emission scenario both approaches project that September ice extent will drop to similar to 1.7 million km(2) in the mid 2040s and reach the ice-free state (defined as 1 million km(2)) in 2054-2058. Under a medium-mitigation scenario, both approaches project a decrease to similar to 1.7 million km(2) in the early 2060s, followed by a leveling off in the ice extent.
引用
收藏
页码:12571 / 12576
页数:6
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