DOI: 10.1029/2004je002354
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Abstract: [1] A new global model for the Martian atmosphere with a vertical domain extending from the surface into the thermosphere (at about 160-180 km) is presented with some preliminary results. The model is a grid point model with a semi-Lagrangian semi-implicit dynamical scheme that is used for weather forecasting by the Meteorological Service of Canada. The physics includes a comprehensive radiative transfer scheme for heating, a boundary and surface layer parameterization. The design of the model allows for diff…

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