The sudden stratospheric warming (SSW) is one of the dramatic dynamical phenomena occurring in the polar region of the winter hemisphere, which is accompanied by changes in the wind and temperature fields (Andrews et al., 1987; Butler et al., 2015; Chandran & Collins, 2014). The interaction between the upward propagation of quasi-stationary planetary waves from the troposphere and the stratospheric mean flow is believed to be the cause of SSW events (Liu & Roble, 2002; Matsuno & Sciences, 1971). Long-term atmospheric data set indicates that SSW events occur rarely in the southern hemisphere (SH), which is most likely due to the weaker planetary wave (PW) forcing and smaller topographical and land-sea differences in the SH. It has been found that the PWs may exhibit anomalous behaviors during SSW periods. For example, Gu, Dou, et al. (2018) and Ma et al. (2017) observed the enhancements of quasi-two-day wave activities during several SSWs. As for the quasi-6-day wave (Q6DW), it also presents an enhancement during some SSWs with either zonal wavenumbers 1 or 2 (Gong et al., 2018; Pancheva et al., 2018). Similarly, the amplification of the quasi-10-day wave may also occur after the collapse of the polar vortex in the stratosphere during some SSW events (