Results 231 to 240 of about 98,238 (279)
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Experimental and theoretical study of internal solitary wave loads on a submerged slender body
Ocean Engineering, 2023Pu Xuan +4 more
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Limiting Forms of Internal Solitary Waves
Journal of Offshore Mechanics and Arctic Engineering, 2002High sensitivity of nonlinear wave structures in the weakly stratified fluid with respect to small perturbations of density in the upstream flow was pointed out by Benney and Ko, Stud. Appl. Math., 59(3), pp. 187–199. In the present paper the influence of fine scale stratification on one of the limiting forms, namely the plateau-shaped solitary waves ...
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Internal Tide Transformation and Oceanic Internal Solitary Waves
2006The transformation of internal tides, or long internal waves, as they propagate over the variable topography of the continental slope and shelf is discussed. Development of a model to describe this transformation is presented and is based on the Korteweg-de Vries equation.
Peter Holloway +2 more
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Combined effect of topography and rotation on oblique internal solitary wave‐wave interactions
Journal of Geophysical Research: Oceans, 2023C. Yuan +3 more
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Internal solitary wave observations in the Flores Sea using the Himawari-8 geostationary satellite
International Journal of Remote Sensing, 2019The Japanese Meteorological Agency’s geostationary satellite Himawari-8/Advanced Himawari Imager (AHI) images, acquired over the Flores Sea in Indonesia, observed that long internal solitary waves (ISWs) seem to be generated from the Sape Strait, which ...
I. W. G. A. Karang +2 more
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Internal solitary wave generation by the tidal flows beneath ice keel in the Arctic Ocean
Journal of Oceanology and Limnology, 2022Peiwen Zhang, Qun Li, Zhenhua Xu, B. Yin
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Generation, propagation, and breaking of internal solitary waves
Chaos: An Interdisciplinary Journal of Nonlinear Science, 2005Tidal, two-layer flow over topography generates a kink of the interface separating an upstream interfacial elevation from a depression above the topography. Upstream undular bores and solitary waves of large amplitude are generated from the interfacial kink. The waves propagate upstream when the tide turns.
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