Article ID Journal Published Year Pages File Type
8059520 Coastal Engineering 2018 9 Pages PDF
Abstract
It is shown that both suspended load transport and tidal asymmetry reduce the equilibrium sand wave height. A residual current results in asymmetrical bed forms that migrate in the direction of the residual current. The combination of suspended load transport and tidal asymmetry results in predicted equilibrium wave heights comparable to wave heights found in the field.
Related Topics
Physical Sciences and Engineering Engineering Ocean Engineering
Authors
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