This letter reports on wavelet spectral analysis of collocated time‐series of streamwise wind speed and aeolian sand transport collected at 0.04 m above the bed in a field experiment on top of a large sand mound in a desert environment. Results suggest three distinct spatio‐temporal scales of interaction between boundary layer turbulence and sediment transport: a long‐term scale associated with the regional mixing layer, an integral time‐scale associated with the internal boundary layer, and a streamer scale associated with the inertial subrange (eddy cascade) and saltation inertia.
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Andreas C. W. Baas (2006) studied this question.
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