Prolonged Quasi‐6‐Day Wave Activities in the Northern Hemisphere MLT Region Due To Antarctic Stratospheric Minor Warming Around September Equinox of 2013 and 2014.

The geopotential height observations from the Aura Microwave Limb Sounder show that the quasi‐6‐day wave (Q6DW) events with westward zonal wavenumber 1 (W1) in the Northern Hemisphere (NH) mesosphere and lower thermosphere (MLT) during September 2013 and 2014 had a prolonged lifetime of ∼45–50 days and reached their maximum amplitudes after the September equinox, while the climatological Q6DW‐W1 is completely dissipated in the background atmosphere before the equinoxes. The Eliassen‐Palm flux diagnostic results indicate that Q6DW‐W1 during September 2013 and 2014 obtained an additional source at ∼60°‐80°S and ∼40–50 km as the September equinox approached, which is related to the baroclinic/barotropic instability in this region. Further investigation on the background atmosphere reveals that several stratospheric minor warming (SMW) events occurred in the Antarctic region during September 2013 and 2014 due to the enhancement of wavenumber 1 activities, accompanied by the increase in the stratospheric temperature, changes in the shape of the polar vortex and the reversal in the zonal mean circulation. The strong planetary wave breaking during the September 2013 and 2014 Antarctic SMW events significantly weakened the strength of the polar night jet (PNJ) and made its peak height descend below ∼35 km, which generated the baroclinic/barotropic instability at the new upper boundary of the PNJ (∼60°‐80°S and ∼40–50 km) by an anomalous double‐jet configuration in the background winds. This unusual instability provided additional wave source and energy for the trans‐equatorial propagation of Q6DW‐W1, which finally led to prolonged wave activities in the NH MLT region. Plain Language Summary: Previous studies have suggested that sudden stratosphere warming (SSW) during wintertime can additionally trigger large‐amplitude traveling planetary waves (PWs) in the mesosphere and lower thermosphere (MLT) region. However, due to the lower occurrence rate and intensity, there are few opportunities to study the impact of Southern Hemisphere (SH) stratospheric warming on global PW behaviors, especially for the climatological event of the eigenmode in the Earth's atmosphere. The Aura satellite observations show that the third climatological event of quasi‐6‐day wave (Q6DW) with westward zonal wavenumber 1 (W1) over one year had an exceptionally long duration in the Northern Hemisphere (NH) MLT region in 2013 and 2014, and abnormally peaked after the September equinox, which is not observed in other years since 2004. The reanalysis data confirms that the stratospheric minor warming (SMW) events occurred over the Antarctic region during September 2013 and 2014, which generated instability under an unusual double‐jet structure in the background winds to provide additional energy for the extension of Q6DW‐W1. The current results establish the relationship between the abnormal PW activities in the NH MLT region and the Antarctic SMW events and provide the first observational evidence that the double‐jet structure can influence the westward propagating PW. Key Points: The duration of the quasi‐6‐day wave (Q6DW) with s = 1 (W1) in the Northern Hemisphere (NH) was greatly extended in September 2013 and 2014The Antarctic stratospheric minor warmings provided additional wave sources to disrupt the typical dissipation pattern of Q6DW‐W1 in the NHThe impact of the double‐jet structure in the Southern Hemisphere on the behavior of westward propagating planetary waves is first observed [ABSTRACT FROM AUTHOR]