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- W2058994920 abstract "The bottom sediment resuspension is an important process in Cleveland Bay, North Australia. Hydrodynamics and suspended sediment concentrations (SSC) were measured from January to April 1993. During this field work, two high sediment resuspension events were observed. An iterative method of calculating the bottom shear stress under wave-current motion has been applied. Using the calculated bottom shear stresses the resuspension mechanisms of bottom sediment in Cleveland Bay has been investigated by analysing data collected during two periods in January and March 1993. Swell has been found to be the most important factor in sediment suspensions for both high SSC events. Wind waves have little effect on SSC levels. Tidal currents are too weak to stir up bottom sediment particles into the flow, but affect the detailed SSC structure by tidal convection. The critical shear stress for sediment resuspension in Cleveland Bay is about 2.0 N/m2." @default.
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- W2058994920 date "1996-12-01" @default.
- W2058994920 modified "2023-10-16" @default.
- W2058994920 title "Wave-current bottom shear stresses and sediment resuspension in Cleveland Bay, Australia" @default.
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- W2058994920 doi "https://doi.org/10.1016/s0378-3839(96)00023-3" @default.
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