Using an objective method to calculate the saltation threshold friction velocity u*t based on measurements using a sand particle counter, the values of u*t were determined to be 0.48 and 0.56 m s-1 under dry (θv = 0.002 m3 m-3) and wet (θv = 0.009 m3 m-3) conditions, respectively, at a gobi site in the Taklimakan Desert. This result shows that u*t increased when soil moisture increased resulting from snowfall in March 2003. A simple relationship was found between the saltation flux q(z) at a reference height z and friction velocity u* and u*t.
CITATION STYLE
Ishizuka, M., Mikami, M., Yamada, Y., & Zeng, F. J. (2009). Threshold friction velocities of saltation sand particles for different soil moisture conditions in the Taklimakan Desert. Scientific Online Letters on the Atmosphere, 5(1), 184–187. https://doi.org/10.2151/sola.2009-047
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