Nonmigrating tides in the thermosphere of Mars

[1] The vertical propagation of nonmigrating (i.e., longitude-dependent or non-Sun-synchronous) solar diurnal and semidiurnal tides into the thermosphere of Mars is investigated through numerical simulation. The waves are generated in the NASA Ames Mars general circulation model (MGCM) through solar radiative, topographic, and nonlinear processes using a comprehensive physics package and including a diurnal cycle. At an altitude near 70 km, zonal wave number decompositions of the diurnal and semidiurnal tidal fields are performed, and each wave component is extended from 70 to 250 km using a linear steady state global scale wave model for Mars (Mars GSWM). Conditions representative of aerocentric longitudes L-s = 30 (near equinox) and L-s = 270 (Southern Hemisphere summer solstice) are considered. Modeled total relative density variations of order +/-10-40% near 125 km are analyzed in terms of the zonal wave numbers (k(s)) seen from the Sun-synchronous perspective of the Mars Global Surveyor (MGS) accelerometer experiment, and yield reasonable agreement in amplitude and phase with the density measurements. The model indicates the two most important waves responsible for k(s) = 3 to be the eastward-propagating diurnal and semidiurnal oscillations with zonal wave numbers s = 2 (similar to15-40%) and s = 1 (similar to8%), respectively. The eastward-propagating diurnal component with s = 1 (similar to15%) and the semidiurnal standing (s = 0) oscillation (similar to4-23%) are concluded to be the main contributors to the k(s) = 2 longitudinal density variation seen from the Mars Global Surveyor (MGS). The standing (s = 0) diurnal oscillation (similar to4-5%) and the westward-propagating semidiurnal component with s = 1 (similar to5-8%) emerge as the most likely contributors to k(s) = 1. Other waves that may make important secondary contributions include the westward-propagating semidiurnal oscillations with s = 3 (similar to4-6%) and s = 4 (similar to3-9%). In addition, above 100 km the wind and temperature fields associated with the above waves represent similar to15-30% perturbations on the Sun-synchronous wind and temperature fields driven in situ by EUV and near-IR solar radiation absorption. Nonmigrating tides primarily arise from zonal asymmetries in wave forcing associated with Mars' topography; our results show for the first time that the dynamical effects of Mars' topography extend throughout the atmospheric column to Mars' exobase (similar to200-250 km).