Abstract
To understand the generation and development mechanism of soil erosion, data of the wind profile from wind tunnel experiments were used, and the characteristics of the turbulent transmission with free stream velocity and the properties of the surfaces in arid and semi-arid regions were studied by the atmospheric aerodynamic method. The result showed that the turbulent momentum fluxes are proportional to the velocity and the roughness of the surfaces. In addition, they are closely related to the density of the roughness elements; the turbulent exchange coefficient over the near surface layer increases with height.
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References
Bian LG, Lu LH, Cheng YJ (2001) Turbulent measurement over the southeastern tibetan plateau. Q J Appl Meteorol 12:1–13
Dong GR, Li Z, Jin J (1987) Some conclusions of erosion. Chin Sci Bull 32:297–301
Li JL, Hong ZX, Luo WD (1999) A study of surface fluxes in Gerze area, Qinghai-Xizang Plateau. Chin J Atmos Sci 23:142–151
Stull RB (1988) An introduction to boundary layer meteorology. Kluwer, Boston, pp 11
Sun JM, Xiao WA, Niu SJ (2002) Turbulent transfer features of the surface layer over desert in a dust and sand weather. J Nanjing Inst Meteorol 25:489–459
Acknowledgments
We gratefully acknowledge the funding from the Knowledge Innovation Project of the Chinese Academy of Science (KZCX3-SW-341), and National Science Fund for Distinguished Young Scholars of the Natural Science Foundation of China (40225003).
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Lü, P., Dong, Z. Wind tunnel experiments on the turbulent transmission over the near surface layer of different surfaces. Environ Geol 50, 983–988 (2006). https://doi.org/10.1007/s00254-006-0267-4
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DOI: https://doi.org/10.1007/s00254-006-0267-4