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Aeolian transport of sedimentary particles is a well-recognized phenomenon in cold regions, but the effect of low temperature (T) and specific humidity (q) upon particle entrainment has not previously been investigated. This study reports on wind-tunnel experiments (-12 °C ≤ T ≤ 32 °C, and 1 g kg-1 ≤ q ≤10 g kg-1) that suggest the aerodynamic drag required to entrain sand sized particles can be 30%...
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