4.6 Editorial Material

Extreme Cold Events from East Asia to North America in Winter 2020/21: Comparisons, Causes, and Future Implications

Journal

ADVANCES IN ATMOSPHERIC SCIENCES
Volume 39, Issue 4, Pages 553-565

Publisher

SCIENCE PRESS
DOI: 10.1007/s00376-021-1229-1

Keywords

extreme weather events; sea surface temperature; Arctic sea ice; Arctic amplification; sudden stratospheric warming; stratospheric polar vortex

Funding

  1. U.S. Department of Energy [DE-SC0020640]
  2. National Natural Science Foundation of China [41675041, 41790475]
  3. Arctic Research Program of the NOAA Global Ocean Monitoring and Observing Office
  4. Deutsche Forschungsgemeinschaft (Transregional Collaborative Research Center ArctiC Amplification: Climate Relevant Atmospheric and SurfaCe Processes, and Feedback Mechanisms (AC)3) [268020496 TRR 172]
  5. Academy of Finland [317999]
  6. Cooperative Institute for Climate, Ocean, & Ecosystem Studies (CIOCES) under NOAA [NA20OAR4320271]

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The three extreme cold weather events were caused by anomalies in three oceans and interactions between Arctic-lower latitude atmospheric circulation processes, influenced by a sudden stratospheric warming event. These events disrupted the stratospheric polar vortex and led to cold air outbreaks, with implications for prediction skill and policy decision making for resilience in One Health, One Future.
Three striking and impactful extreme cold weather events successively occurred across East Asia and North America during the mid-winter of 2020/21. These events open a new window to detect possible underlying physical processes. The analysis here indicates that the occurrences of the three events resulted from integrated effects of a concurrence of anomalous thermal conditions in three oceans and interactive Arctic-lower latitude atmospheric circulation processes, which were linked and influenced by one major sudden stratospheric warming (SSW). The North Atlantic warm blob initiated an increased poleward transient eddy heat flux, reducing the Barents-Kara seas sea ice over a warmed ocean and disrupting the stratospheric polar vortex (SPV) to induce the major SSW. The Rossby wave trains excited by the North Atlantic warm blob and the tropical Pacific La Nina interacted with the Arctic tropospheric circulation anomalies or the tropospheric polar vortex to provide dynamic settings, steering cold polar air outbreaks. The long memory of the retreated sea ice with the underlying warm ocean and the amplified tropospheric blocking highs from the midlatitudes to the Arctic intermittently fueled the increased transient eddy heat flux to sustain the SSW over a long time period. The displaced or split SPV centers associated with the SSW played crucial roles in substantially intensifying the tropospheric circulation anomalies and moving the jet stream to the far south to cause cold air outbreaks to a rarely observed extreme state. The results have significant implications for increasing prediction skill and improving policy decision making to enhance resilience in One Health, One Future.

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