The intensification of winter mid-latitude storm tracks in the Southern Hemisphere

被引:37
|
作者
Chemke, Rei [1 ]
Ming, Yi [2 ]
Yuval, Janni [3 ]
机构
[1] Weizmann Inst Sci, Dept Earth & Planetary Sci, Rehovot, Israel
[2] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA
[3] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA USA
关键词
EXTRATROPICAL CYCLONES; KINETIC-ENERGY; VARIABILITY; CIRCULATION; TRENDS;
D O I
10.1038/s41558-022-01368-8
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Southern mid-latitude winter storms are expected to intensify with emission increases, but it is unknown if such intensification has already emerged. Here, storms are shown to have intensified in recent decades, and current models considerably underestimate this, indicating more risk than projected. The strength of mid-latitude storm tracks shapes weather and climate phenomena in the extra-tropics, as these storm tracks control the daily to multi-decadal variability of precipitation, temperature and winds. By the end of this century, winter mid-latitude storms are projected to intensify in the Southern Hemisphere, with large consequences over the entire extra-tropics. Therefore, it is critical to be able to accurately assess the impacts of anthropogenic emissions on these storms to improve societal preparedness for future changes. Here we show that current climate models severely underestimate the intensification in mid-latitude storm tracks in recent decades. Specifically, the intensification obtained from reanalyses has already reached the model-projected end-of-the-century intensification. The biased intensification is found to be linked to biases in the zonal flow. These results question the ability of climate models to accurately predict the future impacts of anthropogenic emissions in the Southern Hemisphere mid-latitudes.
引用
收藏
页码:553 / +
页数:12
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