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5 - Tidal Residual Flows in Homogeneous, Semienclosed Basins

Published online by Cambridge University Press:  24 February 2022

Arnoldo Valle-Levinson
Affiliation:
University of Florida
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Summary

This chapter describes tidal residual flows expected from dynamic considerations in semienclosed basins without the influence of density gradients. The chapter first qualitatively connects the concepts of Chapter 4, shallow-water tides, to the generation of residual flows. It then introduces a qualitative and quantitative description of the mechanisms that may generate these tidal residual flows in basins with a main channel flanked by shoals. It follows with an explanation of the flow structure in this type of basin, considering ‘long’ and ‘short’ basins, relative to the tidal wavelength. It then depicts examples that compare observations to theoretical expectations. The chapter concludes with descriptions of flows around headlands or sites with coastline curvature.

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Chapter
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Publisher: Cambridge University Press
Print publication year: 2022

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References

Additional Sources

Berthot, A., and Pattiaratchi, C. (2006) Mechanisms for the formation of headland-associated linear sandbanks. Cont. Shelf Res. 26(8): 9871004.CrossRefGoogle Scholar
Geyer, W.R. (1993) Three-dimensional tidal flow around headlands. J. Geophys. Res. 98(C1): 955966.CrossRefGoogle Scholar
Ianniello, J.P. (1977) Tidally induced residual currents in estuaries of constant breadth and depth. J. Mar. Res. 35: 755786.Google Scholar
Ianniello, J.P. (1981) Comments on tidally induced residual currents in estuaries: Dynamics and near bottom flow characteristics. J. Phys. Ocean. 11: 126134.2.0.CO;2>CrossRefGoogle Scholar
Li, C.Y., and O’Donnell, J. (2005) Tidally driven residual circulation in shallow estuaries with lateral depth variation. J. Geophys. Res. 102(C13): 915927, 929.Google Scholar
Signell, R.P., and Geyer, W.R. (1991) Transient eddy formation around headlands. J. Geophys. Res. 96(C2): 25612575.CrossRefGoogle Scholar
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