The Trajectory Towards a Seasonally Ice-Free Arctic Ocean

被引:79
|
作者
Notz, Dirk [1 ]
Stroeve, Julienne [2 ,3 ]
机构
[1] Max Planck Inst Meteorol, Hamburg, Germany
[2] UCL, London, England
[3] Natl Snow & Ice Data Ctr, Boulder, CO USA
来源
CURRENT CLIMATE CHANGE REPORTS | 2018年 / 4卷 / 04期
关键词
Sea ice; Arctic ocean; Future climate; Climate models; Global warming targets; SUMMER SEA-ICE; CLIMATE; CMIP5; FUTURE; CO2; RETREAT; VARIABILITY; ALGORITHMS; IMPACT; CYCLE;
D O I
10.1007/s40641-018-0113-2
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Purpose of Review The observed substantial loss of Arctic sea ice has raised prospects of a seasonally ice-free Arctic Ocean within the foreseeable future. In this review, we summarize our current understanding of the most likely trajectory of the Arctic sea-ice cover towards this state. Recent Findings The future trajectory of the Arctic sea-ice cover can be described through a deterministic component arising primarily from future greenhouse gas emissions, and a chaotic component arising from internal variability. The deterministic component is expected to cause a largely ice-free Arctic Ocean during summer for less than 2 degrees C global warming relative to pre-industrial levels. To keep chances below 5 % that the Arctic Ocean will largely be ice free in a given year, total future CO2 emissions must remain below 500 Gt. Summary The Arctic Ocean will become ice free during summer before mid-century unless greenhouse gas emissions are rapidly reduced.
引用
收藏
页码:407 / 416
页数:10
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