Tidal propagation of deep tropical cloud signatures into the thermosphere from TIMED observations

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Thermosphere extension of the Whole Atmosphere Community Climate Model (2010, methodology): “Figure 11 compares the vertical profiles of DE3 zonal wind amplitude and phase (averaged over ±5° latitude) for August obtained from TIMED SABER and TIDI using a Hough Mode Extension (HME) fitting method [Oberheide and Forbes, 2008] and WACCM‐X.”
Internal wave coupling processes in Earth's atmosphere (2014, unknown): “Usually, monthly mean tidal amplitudes and phases are derived from the observed temperature and zonal and meridional winds, and density residuals (Oberheide and Forbes, 2008a,b).”
Seasonal and quasi‐biennial variations in the migrating diurnal tide observed by Thermosphere, Ionosphere, Mesosphere, Energetics and Dynamics (TIMED) (2009, unknown): “One technique to extract additional information using theory together with wind observations was described by Svoboda et al. [2005] and also used by Oberheide and Forbes [2008] .”
Wavenumber‐4 patterns of the total electron content over the low latitude ionosphere (2008, unknown): “In addition, the observation from the TIMEDSEBER indicates that the seasonal change of the temperature fluctuation of DE3 is very similar to that of the zonal wind component [Chen and Lu, 2007; Oberheide and Forbes, 2008].”