Diurnal Kelvin wave in the atmosphere of Mars: Towards an understanding of ’stationary’ density structures observed by the MGS accelerometer
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v027/i021/2000GL011850/2000GL011850.pdf
Reference13 articles.
1. Thermal tides and stationary waves on Mars as revealed by Mars Global Surveyor thermal emission spectrometer;Banfield;J. Geophys. Res.,2000
2. Possible effects of breaking gravity waves on the circulation of the middle atmosphere of Mars;Barnes;J. Geophys. Res.,1990
3. The Mars Thermosphere, II, General circulation with coupled dynamics and composition;Bougher;J. Geophys. Res.,1990
4. Comparative terrestrial planet thermospheres 3. Solar cycle variation of global structure and winds at solstices;Bougher;J. Geophys. Res.,2000
5. Influence of planetary-scale topography on the diurnal thermal tide during the 1971 Martian dust storm;Conrath;J. Atmos. Sci.,1976
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