Mars: Wind friction speeds for particle movement
- 1 August 1976
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 3 (8) , 417-420
- https://doi.org/10.1029/gl003i008p00417
Abstract
Wind friction threshold speeds (V*t) for particle movement were determined in a low pressure boundary layer wind tunnel at an atmospheric pressure of 5.3 mb. The results imply that for comparable pressures on Mars, the minimum V*t is about 2.5 m/sec, which would require free‐stream winds of 50 to 135 m/sec, depending on the character of the surface and the atmospheric conditions. The corresponding wind speeds at the height of the Viking lander meteorology instrument would be about a factor of two less than the free stream wind speed. The particle size most easily moved by winds on Mars is about 160 µm; particles both larger and smaller than this (at least down to about 5 µm) require stronger winds to initiate movement. The results presented here are in general agreement with previously reported values of V*t for particles 12 µm to 300 µm derived from one atmosphere tests, but are inconsistent with values for particles larger than about 300 µm.This publication has 7 references indexed in Scilit:
- Fluid transport on Earth and aeolian transport on MarsPublished by Elsevier ,2002
- Estimates of the wind speeds required for particle motion on MarsIcarus, 1976
- Saltation threshold on Mars: The effect of interparticle force, surface roughness, and low atmospheric densityIcarus, 1976
- Winds on Mars during the Viking season: Predictions based on a general circulation model with topographyGeophysical Research Letters, 1976
- Wind tunnel studies of Martian aeolian processesProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1974
- Aeolian Processes on Mars: Erosive Velocities, Settling Velocities, and Yellow CloudsGSA Bulletin, 1972
- Windblown Dust on MarsNature, 1969