Comparison of bulk water ice clouds in GM3 with SPICAM ice cloud measurements

Details Comparison of bulk water ice clouds in GM3 with SPICAM ice cloud measurements Comparison of bulk water ice clouds in GM3 with SPICAM ice cloud measurements

Dec 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007agufm.p11a0261a&link_type=abstract

American Geophysical Union, Fall Meeting 2007, abstract #P11A-0261

Physics

5704 Atmospheres (0343, 1060)

Scientific paper

The Global Multiscale Mars Model (GM3) has an improved simulation of the water cycle on Mars which includes phase transitions between water vapour and bulk ice particles, eddy and molecular diffusion, gravitational sedimentation and transport between the polar caps, regolith and atmosphere. One year of nadir UV (200-310 nm) measurements from SPICAM have been used to retrieve cloud and dust optical thickness after allowing for Rayleigh and aerosol scattering and surface scattering. For the comparison with GM3 we focus on the tropical cloud belt (Ls 90-150).

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