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MRO aerobraking predicted densities at 120 km as a function of latitude. Density units are kg/km3.
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Prediction of the structure of the martian upper atmosphere for the Mars Reconnaissance Orbiter (MRO) mission


Stephen W. Bougher1, James R. Murphy2, Jared M. Bell1, and Richard W. Zurek3

1Atmospheric, Oceanic, and Space Sciences Department, University of Michigan, Ann Arbor, MI, 48109, USA
2Dept. of Astronomy, New Mexico State University, Las Cruces, NM 88003, USA
3Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA


Citation: Mars 2, 10-20, 2006; doi:10.1555/mars.2006.0002

History: Submitted: April 3, 2006; Reviewed: April 28, 2006; Revised: May 26, 2006; Accepted: May 30, 2006; Published: June 16, 2006

Summary: The Mars Reconnaissance Orbiter (MRO) spacecraft will undergo aerobraking from April through September 2006 in order to achieve the desired mapping orbit. This aerobraking process requires knowledge of the structure of the Mars upper atmosphere, which is provided through General Circulation Model predictions summarized in this paper.

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Last Updated: July 11, 2008
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