Isobath variation and trapping of continental shelf waves

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Nonlinear internal waves over New Jersey’s continental shelf

[1] Ship and mooring data collected off the coast of New Jersey are used to describe the nonlinear internal wave (NLIW) field and the background oceanographic conditions that formed the waveguide on the shelf. The subinertial, inertial, and tidal circulation are described in detail, and the background fluid state is characterized using the coefficients of the extendedKorteweg–deVries equation. ...

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Scattering and Trapping of Obliquely Incident, Low-Mode Internal Tides off a Continental Shelf and Slope

We demonstrate – using linear scattering theory and an idealized, stratified, rotating ocean domain, with a flat bottom deep ocean and a straight continental slope and shelf – that a high-mode (mode 3) Poincare wave incident on the coastal margin can excite large amplitude leaky coastal trapped waves (CTWs) or leaky edge waves along the coastal margin dependent on the frequency and alongshore w...

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Generation and Propagation of Internal Solitary Waves on the Continental Shelf and Slope

There are two principal objectives. The first is to develop and refine amplitude evolution equations of the Korteweg-de Vries type to the point where they can be used as validated models for the propagation of internal solitary waves. The second is to undertake a major re-examination of the generation process, using a combination of theoretical and numerical analyses, and emphasising the distin...

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Energy transformations and dissipation of nonlinear internal waves over New Jersey’s continental shelf

The energetics of large amplitude, high-frequency nonlinear internal waves (NLIWs) observed over the New Jersey continental shelf are summarized from ship and mooring data acquired in August 2006. NLIW energy was typically on the order of 105 Jm−1, and the wave dissipative loss was near 50 W m−1. However, wave energies (dissipations) were ∼10 (∼2) times greater than these values during a partic...

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ژورنال

عنوان ژورنال: Journal of Fluid Mechanics

سال: 2012

ISSN: 0022-1120,1469-7645

DOI: 10.1017/jfm.2012.153