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The cause of the spring strengthening of the Antarctic polar vortex
Affiliation:1. Univ. Bordeaux, I2M,UMR5295, 351 Cours de la Liberation, 33405 Talence, France;2. Institute of Continuous Media Mechanics UB RAS, 1 Acad. Korolev str., 614013 Perm, Russia
Abstract:The stratospheric polar vortex strengthening from late winter to spring plays a crucial role in polar ozone depletion. The Arctic polar vortex reaches its peak intensity in mid-winter, whereas the Antarctic vortex usually strengthens in early spring. As a result, the strong ozone depletion is observed every year over the Antarctic, while over the Arctic short-term ozone loss occasionally occurs in late winter or early spring. However, the cause of such a difference in the life cycles of the Arctic and Antarctic polar vortices is still not completely clear. Based on the ERA-Interim reanalysis data, we show a high agreement between the seasonal variations of temperature in the subtropical lower stratosphere and zonal wind in the subpolar and polar lower stratosphere in the Southern Hemisphere. Thus, the spring strengthening of the Antarctic polar vortex can occur due to the seasonal temperature increase in the subtropical lower stratosphere in this period.
Keywords:Springtime ozone depletion  Stratospheric polar vortices  Subtropical stratosphere  Brewer-Dobson circulation
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