Non-orographic gravity waves drive 280 m/s zonal jet changes in the Martian thermosphere through 1300 m/s/sol momentum divergence from saturation and wind filtering, strongest in the Hadley-cell descending hemisphere.
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High-Latitude Zonal Jets in the Martian Upper Atmosphere Driven by Non-Orographic Gravity Waves
Non-orographic gravity waves drive 280 m/s zonal jet changes in the Martian thermosphere through 1300 m/s/sol momentum divergence from saturation and wind filtering, strongest in the Hadley-cell descending hemisphere.