Zonal winds in the equatorial upper thermosphere: Decomposing the solar flux, geomagnetic activity, and seasonal dependencies

By Huixin Liu, Hermann Lühr, S. Watanabe, W. Köhler, V. Henize, P. Visser. 2006

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How researchers see this paper

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Nonmigrating tidal signals in the upper thermospheric zonal wind at equatorial latitudes as observed by CHAMP (2009, unknown): “In a first study, Liu et al. (2006)”
An update to the Horizontal Wind Model (HWM): The quiet time thermosphere (2015, methodology): “…topic was recently revisited by Lieberman et al. [2013], who compared the diurnal average and migrating tides of longitudinally averaged zonal winds inferred from CHAMP accelerometer data [Liu et al., 2006; Doornbos et al., 2010] with results from the Whole Atmosphere Model (WAM) of Akmaev [2011].”
Density and Winds in the Thermosphere Deduced from Accelerometer Data (2007, unknown): “[14].”
Longitudinal variation of F region electron density and thermospheric zonal wind caused by atmospheric tides (2007, methodology): “The measured accelerations can be used to estimate the thermospheric mass density and cross-track wind [see Liu et al., 2006].”
Thermospheric Density and Wind Determination from Satellite Dynamics (2012, background): “Unlike Jacchia’s models, however, the density in the DTM and MSIS models is not derived from a direct integration with altitude over the temperature profile.”