Energy Fluxes in Coastal Trapped Waves

The calculation of energy flux in coastal trapped wave modes is reviewed in the context of tidal energy pathways near the coast. The significant barotropic pressures and currents associated with coastal trapped wave modes mean that large errors in estimating the wave flux are incurred if only the ba...

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Veröffentlicht in:Journal of physical oceanography 2019-12, Vol.49 (12), p.3061-3068
1. Verfasser: Musgrave, R. C.
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description The calculation of energy flux in coastal trapped wave modes is reviewed in the context of tidal energy pathways near the coast. The significant barotropic pressures and currents associated with coastal trapped wave modes mean that large errors in estimating the wave flux are incurred if only the baroclinic component is considered. A specific example is given showing that baroclinic flux constitutes only 10% of the flux in a mode-1 wave for a reasonable choice of stratification and bathymetry. The interpretation of baroclinic energy flux and barotropic-to-baroclinic conversion at the coast is discussed: in contrast to the open ocean, estimates of baroclinic energy flux do not represent a wave energy flux; neither does conversion represent the scattering of energy from the tidal Kelvin wave to higher modes.
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subjects Barotropic mode
Bathymeters
Bathymetry
Coastal currents
Coasts
Conversion
Decomposition
Energy
Energy flux
Energy transfer
Fluctuations
Fluxes
Gravitational waves
Kelvin waves
Modes
Stratification
Tidal energy
Tidal power
Topography
Trapped waves
Wave energy
Wave power
title Energy Fluxes in Coastal Trapped Waves
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