The Seasonal Variation of the Propagating Diurnal Tide in the Mesosphere and Lower Thermosphere. Part II: The Role of Tidal Heating and Zonal Mean Winds

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On the composite response of the MLT to major sudden stratospheric warming events with elevated stratopause (2016, background): “The altered wind direction in the tropical lower stratosphere may potentially impact PW and their interaction with the winter eastward jet, as well as tidal amplitudes [McLandress, 2002; Sassi et al., 2013].”
Solar tides as revealed by measurements of mesosphere temperature by the MLS experiment on UARS (2006, methodology): “In the region of interest, the model includes non-LTE (local thermodynamic equilibrium) radiative cooling by CO2 as parameterized by McLandress (2002) based on the Canadian Middle Atmosphere Model (CMAM), and eddy diffusion.”
WHOLE ATMOSPHERE MODELING: CONNECTING TERRESTRIAL AND SPACE WEATHER (2011, background): “…QBO) in the middle atmosphere [e.g., Mayr et al., 1997; Scaife et al., 2000], as well as seasonal variations of atmospheric tides in the mesosphere and lower thermosphere (MLT) [e.g., Akmaev et al., 1996, 1997; McLandress, 1997; Mayr et al., 1998; Akmaev, 2001b, 2001c; McLandress, 2002a, 2002b].”
Thermosphere extension of the Whole Atmosphere Community Climate Model (2010, unknown): “…al., 1997; Vincent et al., 1998; Ward et al., 1999; Oberheide and Gusev, 2002; She, 2004; Oberheide et al., 2006; Forbes et al., 2008; Wu et al., 2008a, 2008b; Xu et al., 2009], as well as modeling studies [e.g., Forbes, 1995; Hagan et al., 1995, 1999; McLandress, 2002a, 2002b; Ward et al., 2005].”