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Read, P. L.; Mulholland, D. P.; Montabone, L. and Lewis, S. R.
(2011).
URL: http://meetingorganizer.copernicus.org/EPSC-DPS201...
Abstract
We present results from assimilated analyses of observations from the Mars Global Surveyor Thermal Emission Spectrometer showing evidence for a regular suppression of baroclinic circumpolar storm activity in both hemispheres of Mars around winter solstice. General circulation model simulations are then used to elucidate the structure and possible causes of this suppression, for which the local ‘Eady growth rate’ appears to be a good predictor.