Weakening of the stratospheric polar vortex by Arctic sea-ice loss

Successive cold winters of severely low temperatures in recent years have had critical social and economic impacts on the mid-latitude continents in the Northern Hemisphere. Although these cold winters are thought to be partly driven by dramatic losses of Arctic sea-ice, the mechanism that links sea...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Kim, BM, Son, SW, Min, SK, Jeong, JH, Kim, SJ, Zhang, XD, Shim, T, Yoon, JH
Other Authors: 환경공학부, 11198091
Format: Article in Journal/Newspaper
Language:English
Published: NATURE 2014
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Online Access:https://oasis.postech.ac.kr/handle/2014.oak/13082
https://doi.org/10.1038/NCOMMS5646
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Summary:Successive cold winters of severely low temperatures in recent years have had critical social and economic impacts on the mid-latitude continents in the Northern Hemisphere. Although these cold winters are thought to be partly driven by dramatic losses of Arctic sea-ice, the mechanism that links sea-ice loss to cold winters remains a subject of debate. Here, by conducting observational analyses and model experiments, we show how Arctic sea-ice loss and cold winters in extra-polar regions are dynamically connected through the polar stratosphere. We find that decreased sea-ice cover during early winter months (November-December), especially over the Barents-Kara seas, enhances the upward propagation of planetary-scale waves with wavenumbers of 1 and 2, subsequently weakening the stratospheric polar vortex in mid-winter (January-February). The weakened polar vortex preferentially induces a negative phase of Arctic Oscillation at the surface, resulting in low temperatures in mid-latitudes. open 1 1 167 174 Y scie scopus