Basic flow field in a tidal basin

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Basic flow field in a tidal basin

[1] A simplified model for tidal flow in a basin is presented. The model is based on the assumption of a flat water surface oscillating synchronously in the tidal basin. Under this hypothesis the depth-averaged continuity equation becomes a Poisson equation that can be easily resolved at each instant of the tidal cycle. This formulation, which is particularly valid for small, deep basins, provi...

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ژورنال

عنوان ژورنال: Geophysical Research Letters

سال: 2002

ISSN: 0094-8276

DOI: 10.1029/2001gl013787