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Observed Damping of Barotropic Seiches through Baroclinic Wave Drag in the Gullmar Fjord
Barotropic Seiches Baroclinic Wave Drag Gullmar Fjord
2008/11/18
Baroclinic wave drag, due to internal wave generation at steep topography, is shown to be a mechanism that effectively subdues barotropic seiches in fjords. A two-layer model for a fjord with a sill a...