Modelling aeolian sand transport using a dynamic mass balancing approach
Knowledge of the changing rate of sediment flux in space and time is essential for quantifying surface erosion and deposition in desert landscapes. While many aeolian studies have relied on time-averaged parameters such as wind velocity (U) and wind shear velocity (u.) to determine sediment flux, th...
| Main Authors: | , , , |
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| Format: | Journal article |
| Published: |
Elsevier
2016
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