Validation of martian meteorological data assimilation for MGS/TES using radio occultation measurements
We describe an assimilation of thermal profiles below about 40 km altitude and total dust opacities into a general circulation model (GCM) of the martian atmosphere. The data were provided by the Thermal Emission Spectrometer (TES) on board the Mars Global Surveyor (MGS) spacecraft. The results of t...
Main Authors: | , , , |
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Format: | Journal article |
Language: | English |
Published: |
2006
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