Abstract

Abstract Eight aeolian sand-transport models are evaluated using a field data set and a new approach to estimating shear velocity. The models are those of Bagnold, 1937 , Kawamura, 1951 , Zingg, 1953 , Owen, 1964 , Kadib, 1965 , Hsu, 1971 , Lettau and Lettau, 1978 , Sorensen, 2004 . All of these models predict transport as a function of shear velocity to the third power. Shear velocities are estimated using wind profile data (log-linear slope) with the von Karman constant and with the apparent von Karman parameter and the results of the different approaches are evaluated based on comparison of regression statistics and RMS error. The models were not adjusted to account for sediment moisture content or local surface slope effects. All of the models have about the same statistical explanatory power, so evaluations were made by comparing slopes and intercepts of best fit (least-squares) lines and RMSE. From this basis, we conclude that predictions made with the Bagnold (1937) model best match our observations, with the models of Kadib, 1965 , Hsu, 1971 performing nearly as well. The Lettau and Lettau, 1978 , Kawamura, 1951 model predictions match observations least.

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