2019年和2020年副热带平流层影响下的南极极地涡旋动力学

V. Zuev, E. Savelieva, V. Krupchatnikov, I. Borovko, A. Pavlinsky, O. G. Chkhetiani, E. A. Maslennikova
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引用次数: 0

摘要

近几十年来,南极极地涡旋在春末夏初(11 月至 12 月)有加强的趋势。2020 年南极极地涡旋的动态就是这一趋势的一个很好的例子,当时它一直持续到 12 月的最后一周。相反,在 2019 年,极地涡旋出现了异常提前的解体,平流层出现了轻微的突然变暖。南极极地涡旋的加强(或减弱)是在亚热带低层平流层温度上升(或下降)的条件下,平流层经向温度梯度上升(或下降)的结果。我们考虑了 2019 年和 2020 年春季亚热带低层平流层的温度变化以及南极极地涡旋的相应响应。相对于气候学手段,2019 年 9-10 月和 2020 年 11 月南极极地涡旋的动态与亚热带低层平流层的温度变化基本同步。通过相关性分析,我们表明 12 月的南极极地涡旋动态主要是由于 11 月下半月发生的副热带平流层低层温度变化造成的,这种变化在 2020 年表现出来。
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Antarctic polar vortex dynamics in 2019 and 2020 under the influence of the subtropical stratosphere
The trend of strengthening of the Antarctic polar vortex in late spring and early summer (November–December) has been observed in recent decades. A good example of this trend is the dynamics of the Antarctic polar vortex in 2020 when it existed until the last week of December. In 2019, conversely, on the contrary, an unusually early breakup of the polar vortex occurred, a minor sudden stratospheric warming was recorded. Strengthening (or weakening) of the Antarctic polar vortex occurs as a result of an increase (or decrease) in the stratospheric meridional temperature gradient under conditions of growth (or decline) in the temperature of the lower subtropical stratosphere. We considered the temperature variations in the lower subtropical stratosphere in the spring of 2019 and 2020 and the corresponding response of the Antarctic polar vortex. The dynamics of the Antarctic polar vortex in September–October 2019 and November 2020 was largely synchronized with the temperature changes in the lower subtropical stratosphere relative to climatological means. Using correlation analysis, we show that the Antarctic polar vortex dynamics in December is largely due to the temperature changes in the lower subtropical stratosphere that occurred in the second half of November, which manifested itself in 2020.
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