Comparison of stratospheric evolution during the major sudden stratospheric warming events in 2018 and 2019

IF 2.9 3区 地球科学 Earth and Planetary Physics Pub Date : 2020-09-18 DOI:10.26464/epp2020044
Zheng Ma, Yun Gong, ShaoDong Zhang, JiaHui Luo, QiHou Zhou, ChunMing Huang, KaiMing Huang
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引用次数: 9

Abstract

Using Modern-Era Retrospective analysis for Research and Applications, Version 2 (MERRA-2) data in the northern hemisphere at the 10 hPa level, we compared the stratospheric evolution of temperature and geopotential height during two major sudden stratosphere warming events (SSWs) that occurred in the Arctic winter of 2018 and 2019. In the prewarming period, poleward temperature-enhanced regions were mainly located around 120°E with a displaced vortex and around 120°E and 60°W with splitting vortices. The evolution of geopotential height indicated that these temperature-enhanced regions were both on the western side of high-latitude anticyclones. In the postwarming period, the polar vortex turned from splitting to displacement in the 2018 SSW but from displacement to splitting in the 2019 SSW. Both transitions were observed over the Atlantic region, which may have been caused by anticyclones moving through the polar region. Our findings revealed that the evolution of the anticyclone is important during SSWs and is closely related to temperature-enhanced regions in the prewarming periods and to transitions of the polar vortices in postwarming periods.

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2018年和2019年主要平流层突然变暖事件的平流层演化比较
利用北半球10 hPa水平的现代回顾性分析第2版(MERRA-2)数据,我们比较了2018年和2019年北极冬季发生的两次主要平流层突然变暖事件(SSWs)期间平流层温度和位势高度的演变。在暖前期,极向增温区主要分布在120°E附近的位移涡和120°E和60°W附近的分裂涡。位势高度演化表明,这些增温区均位于高纬反气旋西侧。暖后期极涡在2018年SSW由分裂转向位移,在2019年SSW由位移转向分裂。这两个转变都是在大西洋地区观测到的,这可能是由穿过极地的反气旋引起的。研究结果表明,反气旋的演化与暖前增温区和暖后极涡的转变密切相关。
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来源期刊
Earth and Planetary Physics
Earth and Planetary Physics GEOSCIENCES, MULTIDISCIPLINARY-
自引率
17.20%
发文量
174
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