Global and seasonal distribution of gravity wave activity in Mars' lower atmosphere derived from MGS radio occultation data

Author:

Creasey John E.1,Forbes Jeffrey M.1,Hinson David P.2

Affiliation:

1. Department of Aerospace Engineering Sciences; University of Colorado; Boulder Colorado USA

2. Department of Electrical Engineering; Stanford University; Stanford California USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference16 articles.

1. Baines , P. G. T. N. Palmer 1990 Rationale for a new physically-based parametrization of sub-grid scale orographic effects Tech. Rep. 169 Eur. Cent. for Medium-Range Weather Forecasts Reading, U. K.

2. Mariner 9 observations of the Mars north polar hood;Briggs;Bull. Am. Meteorol. Soc.,1974

3. Gravity wave drag in a global circulation model of the Martian atmosphere: Parametrisation and validation;Collins;Adv. Space. Res.,1997

4. Gravity wave and equatorial wave morphology of the stratosphere derived from long-term rocket soundings;Eckermann;Q. J. R. Meteorol. Soc.,1994

5. Improved general circulation models of the Martian atmosphere from the surface to above 80 km;Forget;J. Geophys. Res.,1999

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