TY - JOUR
T1 - Predicting aeolian sand transport rates
T2 - A reevaluation of models
AU - Sherman, Douglas J.
AU - Li, Bailiang
N1 - Funding Information:
The original field work benefitted from the contributions of many, including financial support from the European Community IMPACTS Project No. EV5V-CT93-0258 , supervised by Julian Orford and Robert Devoy, and the US Fulbright Scholar Program to DJS. Field assistance was rendered by Cathy Delaney Robert Devoy, John McKenna, Charles Roche, and Robert Stewart. The contributions of the coauthors of the 1998 paper, Derek Jackson, Steve Namikas, and Jinkang Wang are gratefully acknowledged. Thanks also to Andreas Baas, Jean Ellis, and an anonymous reviewer for suggestions on how to improve this paper.
PY - 2012/1
Y1 - 2012/1
N2 - 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) and Sørensen (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 Kármán constant and with the apparent von Kármán 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) and Hsu (1971) performing nearly as well. The Lettau and Lettau (1978) and Kawamura (1951) model predictions match observations least.
AB - 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) and Sørensen (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 Kármán constant and with the apparent von Kármán 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) and Hsu (1971) performing nearly as well. The Lettau and Lettau (1978) and Kawamura (1951) model predictions match observations least.
KW - Apparent von Kármán parameter
KW - Bagnold
KW - Lettau and Lettau
KW - Shear velocity
UR - http://www.scopus.com/inward/record.url?scp=84855873652&partnerID=8YFLogxK
U2 - 10.1016/j.aeolia.2011.06.002
DO - 10.1016/j.aeolia.2011.06.002
M3 - Review article
AN - SCOPUS:84855873652
SN - 1875-9637
VL - 3
SP - 371
EP - 378
JO - Aeolian Research
JF - Aeolian Research
IS - 4
ER -