Orographically forced oscillations in a dynamical model of the Martian atmosphere

Computer Science

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Atmospheric Circulation, Atmospheric Models, Mars Atmosphere, Spatial Distribution, Dynamic Models, Forced Vibration, Orography

Scientific paper

The barotropic, orographically-forced intraseasonal oscillations of the Martian atmosphere are presently analyzed by means of a single-layer shallow-water model. An oscillation with 85-Martian day mean period is noted in a time-series of the model global atmospheric angular momentum, and its robustness is verified. The oscillation has a standing zonal component whose centers of action are located upstream and downstream of salient orographic features. A resemblance arises between the oscillation's northern-hemisphere features and those of the terrestrial 40-day oscillation.

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