Sensitivities of Bottom Stress Estimation to Sediment Stratification in a Tidal Coastal Bottom Boundary Layer
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DOI: 10.3390/jmse8040256
Abstract: The bottom friction velocity (U*), which controls seabed erosion and deposition, plays a critical role in sediment transport in tidal coastal bottom boundary layers. Approaches have been proposed to calculate U*, including the log profile… read more here.
Keywords: stratification; sediment stratification; velocity; coastal bottom ... See more keywords