Physics – Computational Physics
Scientific paper
2011-04-14
Physics
Computational Physics
Scientific paper
We reveal a discontinuous transition in the saturated flux for aeolian saltation by simulating explicitly particle motion in turbulent flow. The discontinuity is followed by a coexistence interval with two metastable solutions. The modification of the wind profile due to momentum exchange exhibits a second maximum at high shear strength. The saturated flux depends on the strength of the wind as $q_s=q_0+A(u_*-u_t)(u_*^2+u_t^2)$.
Carneiro M. V.
Herrmann Hans Jürgen
Pähtz Thomas
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