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Radio occultation measurements and MGCM simulations of Kelvin waves on Mars |
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| Authors: | DP Hinson M Pätzold B Häusler GL Tyler |
| Institution: | a Department of Electrical Engineering, Stanford University, Stanford, CA 94305, USA b Institut für Geophysik und Meteorologie, Universität zu Köln, Cologne, Germany c NOAA/Geophysical Fluid Dynamics Laboratory, Princeton University, Princeton, NJ 08542, USA d Institut für Raumfahrttechnik, Universität der Bundeswehr München, Neubiberg, Germany |
| Abstract: | We have derived new results concerning thermal tides on Mars from a combination of radio occultation measurements and numerical simulations by a Mars General Circulation Model (MGCM). This investigation exploits a set of concurrent observations by Mars Express (MEX) and Mars Global Surveyor (MGS) in mid-2004, when the season on Mars was midspring in the northern hemisphere. The MEX occultations sampled the atmosphere near the evening terminator at latitudes ranging from 54° N to 15° S. The MGS occultations provided complementary coverage near the morning terminator at latitudes of 35° N and 71° S. The geopotential field derived from these measurements contains distinctive modulation caused by solar-asynchronous thermal tides. Through careful analysis of the combined observations, we characterized two prominent wave modes, obtaining direct solutions for some properties, such as the amplitude and phase, as well as constraints on others, such as the period, zonal wave number, and meridional structure. We supplemented these observations with MGCM simulations. After evaluating the performance of the MGCM against the measurements, we used the validated simulation to deduce the identity of the two tidal modes and to explore their behavior. One mode is a semidiurnal Kelvin wave with a zonal wave number of 2 (SK2), while the other is a diurnal Kelvin wave with a zonal wave number of 1 (DK1). Both modes are known to be close to resonance in the martian atmosphere. Our observations of the SK2 are more complete and less ambiguous than any previous measurement. The well-known DK1 is the dominant solar-asynchronous tide in the martian atmosphere, and our results confirm and extend previous observations by diverse instruments. |
| Keywords: | Mars atmosphere Atmospheres dynamics |
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