“…Although major SSW events are rare in the Antarctic region, stratospheric minor warming (SMW) events are more frequent in the SH during wintertime (Alajmi et al.,
1985; Coy et al.,
2005; Hirota et al.,
1990; Laat & Weele,
2011; Shiotani et al.,
1993; Vincent et al.,
2022), which may also lead to large‐scale anomalies in the background atmosphere to influence traveling PW activities in the MLT region. In this paper, the specific criteria for the Antarctic SMW events are as follows (Vincent et al.,
2022): (a) Warmings at 60°–90°S and 10 hPa and increase in the meridional temperature gradient ([
(80°–90°S)‐
(60°–70°S)]/20°) at 10 hPa; (b) The deceleration in the zonal mean zonal wind at 60°S at any level from 10 hPa to 0.01 hPa (the wind reversal is not required). In addition, changes in the morphology of the polar vortex and residual circulation can be regarded as additional evidence for the occurrence of SMW.…”