与冬季急流有关的电离层和平流层短周期变率

A. Yasyukevich, A. Vesnin
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摘要

在本研究中,我们对电离层和平流层短周期变率的时空动态进行了联合分析。我们分析了2008-2009年、2012-2013年和2018-2019年冬季发生强烈的冬至平流层突然变暖(SSW)的时期。在安静的冬季,平流层变率指数在40-65°N的有限纬向间隔内增加。在SSW条件下,平流层扰动停止产生,平流层扰动指数下降。该指数保持低位的时间最长可达一个月。电离层TEC变率指数vrTEC的纬时分布也表现出类似的动态特征。在平流层开始SSW后,电离层变率水平降低。短周期电离层变率的减少可以用平流层中波浪产生的减少来解释,这与在南纬向风期间急流的破坏有关。
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Short-period variability in the ionosphere and the stratosphere related to winter jet stream
In the study, we carried out a joint analysis of the spatio-temporal dynamics of ionospheric and stratospheric short-period variability. We analyze the periods of winters of 2008–2009, 2012–2013, and 2018–2019, when strong midwinter sudden stratospheric warmings (SSW) occurred. During quiet winter periods, the stratospheric variability index is shown to be increased at a limited latitudinal interval of 40-65°N. Under SSW condition, the generation of disturbances in the stratosphere stops and a decrease in the stratosphere disturbance index appears. The index keeps low values for up to a month. The latitudinal-temporal distributions of the ionospheric TEC variability index vrTEC also show similar dynamics. The level of ionospheric variability decreases after the SSW onset in the stratosphere. The decrease in the short-period ionospheric variability can be explained by reduction of wave generation in the stratosphere, associated with the destruction of the jet stream during SSW periods.
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