Record warming at the South Pole during the past three decades

被引:127
作者
Clem, Kyle R. [1 ]
Fogt, Ryan L. [2 ]
Turner, John [3 ]
Lintner, Benjamin R. [4 ]
Marshall, Gareth J. [3 ]
Miller, James R. [4 ]
Renwick, James A. [1 ]
机构
[1] Victoria Univ Wellington, Sch Geog Environm & Earth Sci, Wellington, New Zealand
[2] Ohio Univ, Dept Geog, Athens, OH 45701 USA
[3] British Antarctic Survey, Nat Environm Res Council, Cambridge, England
[4] Rutgers State Univ, New Brunswick, NJ USA
基金
英国自然环境研究理事会; 美国国家科学基金会;
关键词
ANTARCTIC SEA-ICE; CLIMATE-CHANGE; SURFACE; HEMISPHERE; TEMPERATURE; PENINSULA; IMPACTS; TRENDS; OSCILLATION; SIGNATURES;
D O I
10.1038/s41558-020-0815-z
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Over the last three decades, the South Pole has experienced a record-high statistically significant warming of 0.61 +/- 0.34 degrees C per decade, more than three times the global average. Here, we use an ensemble of climate model experiments to show this recent warming lies within the upper bounds of the simulated range of natural variability. The warming resulted from a strong cyclonic anomaly in the Weddell Sea caused by increasing sea surface temperatures in the western tropical Pacific. This circulation, coupled with a positive polarity of the Southern Annular Mode, advected warm and moist air from the South Atlantic into the Antarctic interior. These results underscore the intimate linkage of interior Antarctic climate to tropical variability. Further, this study shows that atmospheric internal variability can induce extreme regional climate change over the Antarctic interior, which has masked any anthropogenic warming signal there during the twenty-first century. Surface air temperatures at the South Pole warmed at over three times the global rate in recent decades. Research shows this trend was driven remotely by the tropics and locally by a positive phase of the Southern Annular Mode, increasing the influx of warm moist air atop anthropogenic warming.
引用
收藏
页码:762 / +
页数:18
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