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Eulerian Volume Transport Induced by Spatially Damped Internal Equatorial Kelvin Waves
Publisher: American Meteorological Society
Abstract: he Eulerian volume transport in internal equatorial Kelvin waves subject to viscous attenuation is investigated theoretically by integrating the horizontal momentum equations in the vertical. In terms of small perturbations, ...
Mass Transport in the Stokes Edge Wave for Constant Arbitrary Bottom Slope in a Rotating Ocean
Publisher: American Meteorological Society
Abstract: he Lagrangian mass transport in the Stokes surface edge wave is obtained from the vertically integrated equations of momentum and mass in a viscous rotating ocean, correct to the second order in wave steepness. The analysis ...
Stokes Drift in Internal Equatorial Kelvin Waves: Continuous Stratification versus Two-Layer Models
Publisher: American Meteorological Society
Abstract: he Stokes drift in long internal equatorial Kelvin waves is investigated theoretically for an inviscid fluid of constant depth. While the Stokes drift in irrotational waves is positive everywhere in the fluid, that is, ...
Dispersion Relation for Continental Shelf Waves When the Shallow Shelf Part Has an Arbitrary Width: Application to the Shelf West of Norway
Publisher: American Meteorological Society
Abstract: he dispersion relation for continental shelf waves (CSWs) in a shelf region with an unbounded flat outer ocean, a convex-upward exponential shelf, and an interior flat region of arbitrary width D is derived. The calculations ...
Eulerian versus Lagrangian Approaches to the Wave-Induced Transport in the Upper Ocean
Publisher: American Meteorological Society
Abstract: It is demonstrated that the Eulerian and the Lagrangian descriptions of fluid motion yield the same form for the mean wave-induced volume fluxes in the surface layer of a viscous rotating ocean. In the Eulerian case, the ...
A Quasi-Eulerian, Quasi-Lagrangian View of Surface-Wave-Induced Flow in the Ocean
Publisher: American Meteorological Society
Abstract: In this study the influence of surface waves on the mean flow in an ocean of arbitrary depth is examined. The wave-induced forcing on the mean flow is obtained by integrating the Eulerian equations for mass and momentum ...