Case studies of the mesospheric response to recent minor, major, and extended stratospheric warmings

By D. Siskind, Stephen D. Eckermann, J. McCormack, L. Coy, K. Hoppel, N. Baker. 2010

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On the composite response of the MLT to major sudden stratospheric warming events with elevated stratopause (2016, background): “GW [Holton, 1983; Siskind et al., 2010].”
Equatorial and Low Latitude Ionospheric Effects During Sudden Stratospheric Warming Events (2011, background): “These mesospheric changes result from both planetary wave and gravity wave forcing (Siskind et al. 2010; Yamashita et al. 2010a, 2010b).”
Sudden Stratospheric Warmings (2020, background): “The stratopause often reforms at high altitudes ( ∼ 70-80 km) after SSW events, fol-818 lowed by a gradual descent to its climatological altitude of ∼ 50–55 km over the ensu-819 ing 2-3 weeks (Manney et al., 2008; Siskind et al., 2010).”
WHOLE ATMOSPHERE MODELING: CONNECTING TERRESTRIAL AND SPACE WEATHER (2011, result): “Consistent with observations and other simulations, the warming in the polar stratosphere by about 30 K was accompanied by a mesospheric cooling [Liu and Roble, 2002; Coy et al., 2005; Siskind et al., 2005, 2010].”