Identifying a human signal in the North Atlantic warming hole

被引:54
|
作者
Chemke, Rei [1 ]
Zanna, Laure [2 ,3 ]
Polvani, Lorenzo M. [1 ,4 ,5 ]
机构
[1] Columbia Univ, Dept Appl Phys & Appl Math, New York, NY 10027 USA
[2] Univ Oxford, Dept Phys, Atmospher Ocean & Planetary Phys, Oxford, England
[3] NYU, Courant Inst Math Sci, New York, NY USA
[4] Columbia Univ, Dept Earth & Environm Sci, Palisades, NY USA
[5] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY USA
基金
美国国家科学基金会;
关键词
CMIP5;
D O I
10.1038/s41467-020-15285-x
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
North Atlantic sea surface temperatures have large climate impacts affecting the weather of the Northern Hemisphere. In addition to a substantial warming over much of the North Atlantic, caused by increasing greenhouse gases over the 21st century, climate projections show a surprising region of considerable future cooling at midlatitudes, referred to as the North Atlantic warming hole. A similar pattern of surface temperature trends has been observed in recent decades, but it remains unclear whether this pattern is of anthropogenic origin or a simple manifestation of internal climate variability. Here, analyzing state-of-the-art climate models and observations, we show that the recent North Atlantic warming hole is of anthropogenic origin. Our analysis reveals that the anthropogenic signal has only recently emerged from the internal climate variability, and can be attributed to greenhouse gas emissions. We further show that a declining northward oceanic heat flux in recent decades, which is linked to this surface temperature pattern, is also of anthropogenic origin.
引用
收藏
页数:7
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