This paper presents a contemporary review of vertical coupling in the atmosphere and
ionosphere system induced by internal waves of lower atmospheric origin. Atmospheric …

Gravity waves are primarily generated in the lower atmosphere, and can reach
thermospheric heights in the course of their propagation. This paper reviews the recent …

Abstract The high‐resolution Whole Atmosphere Community Climate Model with
thermosphere/ionosphere extension (WACCM‐X) is used to study the impacts of gravity …

First high‐altitude observations of gravity wave (GW)‐induced CO2 density perturbations in
the Martian thermosphere retrieved from NASA's Neutral Gas Ion Mass Spectrometer …

Wavelike perturbations in the Martian upper thermosphere observed by the Neutral Gas Ion
Mass Spectrometer (NGIMS) onboard the Mars Atmosphere and Volatile EvolutioN …

Using a ground‐to‐exosphere general circulation model for Mars we have simulated the
variability of the dayside temperatures at the exobase during eight Martian years (MY, from …

Our recently developed nonlinear spectral gravity wave (GW) parameterization has been
implemented into a Martian general circulation model (GCM) that has been extended to∼ …

In order to study the dynamical role of gravity waves (GWs) propagating upward from the
lower atmosphere to the thermosphere, numerical simulation using a high‐resolution …

Gravity waves (GWs) are important for vertical coupling between the lower and upper
atmosphere on Mars. Saturated GWs will promote the acceleration of mean flow and …

We analyze quiet‐time data from the Gravity Field and Ocean Circulation Explorer satellite
as it overpassed the Southern Andes at z≃ 275 km on 5 July 2010 at 23 UT. We extract the …