2025/12/11 by Chavez, Jose A. Perez, Tucker, Orenthal J., Mogan, Shane R. Carberry +2
Physics and Astronomy · Mathematics · Earth and Planetary Sciences · #Planetary Science and Exploration #Gas Dynamics and Kinetic Theory #Seismic Waves and Analysis
paper · doi:10.48550/arxiv.2512.10887
Direct Simulation Monte Carlo (DSMC) calculations of acoustic gravity wave propagation into the exobase region of a Mars-like atmosphere reveal that radial geometry can reduce wave-driven heating compared to a Cartesian model. We examine two acoustic wave (AW) modes with periods of 11 minutes (AW1) and 5.5 minutes (AW2) propagating from 100 to 320 km altitude using a radial molecular kinetics model. The wave-driven heating was reduced by 40-56% with cycle-averaged temperature gradient ⟨ dT/dr ⟩ decreasing from 9.4 K per scale height H0 to 5.6 K/H0 for AW1 and from 4.4 K/H0 to 1.9 K/H0 for AW2 when accounting for planetary curvature. While the growth in wave density amplitude was attenuated for the 1D radial geometry as well, the heating differences are more pronounced, with both effects driven by geometric spreading accumulating as waves propagate into increasingly rarefied regions. These findings suggest that accounting for curvature effects is crucial when conducting DSMC estimates of acoustic wave contributions to thermospheric heating and atmospheric escape, as Cartesian-based derived counterparts may be overestimated by factors of 1.7-2.3 for these frequencies.