Modeling aeolian surface interaction phenomena at Nili and Meroe Paterae

Details Modeling aeolian surface interaction phenomena at Nili and Meroe Paterae Modeling aeolian surface interaction phenomena at Nili and Meroe Paterae

Oct 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011epsc.conf.1617m&link_type=abstract

EPSC-DPS Joint Meeting 2011, held 2-7 October 2011 in Nantes, France. http://meetings.copernicus.org/epsc-dps2011, p.1617

Physics

Scientific paper

Repeat high-resolution imagery is beginning to yield examples of contemporary (even intraseasonal) sandsized sediment transport on Mars. A mesoscale regional climate model is used to investigate the atmospheric flows that may responsible for observations of such sand-sized sediment transport within Nili Patera. The simulations suggest that strong topographic enhancement of regional-scale flows occurs, likely resulting in significant sediment transport only in certain seasons, and for short periods of time each day.

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