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Validation of martian meteorological data assimilation for MGS/TES using radio occultation measurements

Abstract:

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 the assimilation are verified against an independent source of contemporaneous data represented by radio occultation measurements with an ultra-stable radio oscillator, also aboard MGS. This paper d...

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Publication status:
Published

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Publisher copy:
10.1016/j.icarus.2006.07.012

Authors


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Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Role:
Author
Journal:
ICARUS More from this journal
Volume:
185
Issue:
1
Pages:
113-132
Publication date:
2006-11-01
DOI:
EISSN:
1090-2643
ISSN:
0019-1035
Language:
English
Keywords:
Pubs id:
pubs:5982
UUID:
uuid:1a878ede-5a42-47fb-82e4-7a761ad95650
Local pid:
pubs:5982
Source identifiers:
5982
Deposit date:
2012-12-19

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