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The effect of a global dust storm on simulations of the Martian water cycle

Böttger, H.M.; Lewis, S.R.; Read, P.L. and Forget, F. (2004). The effect of a global dust storm on simulations of the Martian water cycle. Geophysical Research Letters, 31 L22702.

DOI (Digital Object Identifier) Link: http://dx.doi.org/10.1029/2004GL021137
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Abstract

Recent Mars Global Surveyor Thermal Emission Spectrometer (TES) observations have shown the effects of a global dust storm on the water cycle on Mars. Simulations using a Mars General Circulation Model were conducted to assess the influence of an arbitrary global dust storm on the modelled water cycle. Further, the effects of an adsorbing regolith during the dust storm were examined. Both with an active and a passive regolith the water cycle is substantially affected during the course of the dust storm, but returns to ambient conditions soon after the storm has abated. Differences between the simulations do exist, especially in the southern hemisphere during summer. When comparing the simulations with observations both the active and passive regolith simulations fail to fully replicate the general trends observed by TES. However, the actions of an adsorbing regolith appear to result in a water cycle more closely resembling the observations.

Item Type: Journal Article
Copyright Holders: 2004 by the American Geophysical Union
ISSN: 0094-8276
Academic Unit/Department: Science > Physical Sciences
Interdisciplinary Research Centre: Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)
Item ID: 4925
Depositing User: Users 6041 not found.
Date Deposited: 14 Jul 2006
Last Modified: 04 Jul 2011 14:04
URI: http://oro.open.ac.uk/id/eprint/4925
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