Abstract
The response of a continental shelf to incident Poincaré waves in a homogeneous ocean rotating about a vertical axis is considered, linear friction being incorporated in the model. The shelf is shown to resonate at the usual 'quarter-wavelength' frequencies, but surprisingly, the maximum energy absorption at resonance occurs for a particular value of the relation between the friction parameter and the shelf geometry.
Subject
Ecology,Aquatic Science,Ecology, Evolution, Behavior and Systematics,Oceanography
Cited by
12 articles.
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