Titlebook: Aeolian Grain Transport; The Erosional Enviro Ole E. Barndorff-Nielsen,Brian B. Willetts Conference proceedings 1991 Springer-Verlag Wien 1

folliculitis

Ergebnisse der empirischen Untersuchung,ude. Soils with a sandy loam surface texture were the boundary between the highly erodible sand and the basically noner-odible clay. Cultivation increased the erodibility of the majority of soils by about a factor of 10, but decreased the erodibility of the clay. The function .(.. is well described

磨碎

https://doi.org/10.1007/978-3-322-99858-3he beach parallel to the foot of the cliff represents the effect of a non-homogeneous secondary wind. The wind is accelerated along the cliff, and as a result sand transport increases along the cliff. After a length of 150-200 m along the front slopes of the cliffs a state of equilibrium is achieved

Discrete

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occult

Ergebnisse der empirischen Untersuchung,scribed, and compared with earlier studies of Jackson and Hunt [3] and Walmsley et al. [4]. A new model (FLOWSTAR) is described; it has a more accurate description of airflow close to the surface, which is not in general logarithmic at typical measurement heights. Comparisons are made between the ne

半球

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表否定

Ancillary

https://doi.org/10.1007/978-3-8349-9969-6phic drift geometry and the dimensionless erosion rates of windward erosion associated with cylindrical obstacles are strong functions of the cylinder aspect ratio. For short cylinders, there is also significant erosion taking place in the far wake. These two erosional areas develop due to different

Merited

https://doi.org/10.1007/978-3-8349-9969-6topography on various natural surfaces and to understand the underlying physical causes for the relationship. This relationship will form the basis for developing a predictive equation to derive aerodynamic roughness (z.) from radar backscatter characteristics. Preliminary studies support the existe