Mars 5, 159-171, 2010 | doi:10.1555/mars.2010.0007
Submitted: May 15, 2010; Reviewed: July 2, 2010; Revised: August 16, 2010; Accepted: August 27, 2010; Published: December 10, 2010
Daytime convectively-driven boundary layer turbulence produces structures on scales smaller than a few kilometers that can only be resolved in modeling by large-eddy simulations (LES). We have run several LES using the Mars Regional Atmospheric Modeling System and present fits of friction velocity to a two-parameter Weibull distribution for use with lower resolution models.
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