Role of sea ice in formation of wintertime arctic temperature anomalies

被引:10
作者
Semenov, V. A. [1 ,2 ,3 ]
机构
[1] Russian Acad Sci, Obukhov Inst Atmospher Phys, Moscow 119017, Russia
[2] Shirshov Inst Oceanol, Moscow 117997, Russia
[3] Helmholtz Ctr Ocean Res Kiel GEOMAR, D-24105 Kiel, Germany
基金
俄罗斯基础研究基金会;
关键词
Arctic climate; climate models; ice cover; climate variability; NORTH-ATLANTIC OSCILLATION; SURFACE AIR-TEMPERATURE; CLIMATE-CHANGE; VARIABILITY; HEMISPHERE; CIRCULATION; TRENDS; IMPACT; PERIOD; COVER;
D O I
10.1134/S0001433814040215
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Numerical experiments with the ECHAM5 atmospheric general circulation model (AGCM) using the empirical HadISST1.1 data on sea surface temperature (SST) and sea ice concentration (SIC) in the 20th century as boundary conditions are analyzed. The experiments show that the model correctly reproduces the wintertime Arctic warming in the last 30 years of the 20th century but is unable to reproduce mid-20th century warming. Because the wintertime Arctic surface air temperature changes are closely related to SIC anomalies, it is assumed that one reason for this discrepancy is the lack of a negative SIC anomaly in the prescribed boundary conditions during a mid-20th century warm period. It is also shown that the model with-out prescribed ice cover changes does not reproduce a temperature trend in the Arctic in recent 30 years of the 20th century. The experimental results indicate that the mid-20th century warming was accompanied by a significant negative anomaly of the wintertime Arctic sea ice extent comparable to current trends and also point to a considerable contribution of natural variability to modern climate changes.
引用
收藏
页码:343 / 349
页数:7
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