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

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31#
發(fā)表于 2025-3-27 00:14:25 | 只看該作者
32#
發(fā)表于 2025-3-27 02:40:07 | 只看該作者
Air flow and sand transport over sand-dunes,d different sets of measurements over a dune, by Howard and Walmsley [5], and by our group in recent field measurements over a dune in Oman, and in a new wind-tunnel study of Howard’s dune. It is found that the FLOWSTAR calculations agree well with these sets of measurements upwind of the brink. Sin
33#
發(fā)表于 2025-3-27 07:29:38 | 只看該作者
Cross-shore selective sorting processes and grain size distributional shape, along the -0.6 to -0.7 . lines. However, this group is divided into two basically different depositional environments: water-lain backshore populations dominated by the swash-backwash bidirectional sheet flow and wind-blown sand originating from the backshore sediments. The different grain-size pop
34#
發(fā)表于 2025-3-27 11:20:17 | 只看該作者
Assessment of aerodynamic roughness via airborne radar observations,sensitivity of the relationship to microwave parameters using calibrated multiple wavelength, polarization, and incidence angle aircraft radar data, and 3) applying the results to models to gain an understanding of the physical properties which produce the relationship. The approach combines the mea
35#
發(fā)表于 2025-3-27 17:26:54 | 只看該作者
36#
發(fā)表于 2025-3-27 19:35:48 | 只看該作者
The effect of sea cliffs on inland encroachment of aeolian sand,he 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
37#
發(fā)表于 2025-3-28 00:48:22 | 只看該作者
38#
發(fā)表于 2025-3-28 02:10:17 | 只看該作者
39#
發(fā)表于 2025-3-28 06:36:03 | 只看該作者
Ergebnisse der empirischen Untersuchung, along the -0.6 to -0.7 . lines. However, this group is divided into two basically different depositional environments: water-lain backshore populations dominated by the swash-backwash bidirectional sheet flow and wind-blown sand originating from the backshore sediments. The different grain-size pop
40#
發(fā)表于 2025-3-28 11:36:24 | 只看該作者
https://doi.org/10.1007/978-3-8349-9969-6sensitivity of the relationship to microwave parameters using calibrated multiple wavelength, polarization, and incidence angle aircraft radar data, and 3) applying the results to models to gain an understanding of the physical properties which produce the relationship. The approach combines the mea
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