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Titel Stationary solutions of the extended reduced Ostrovsky equation
VerfasserIn Maria Obregon, Ramon Fernandez-Feria, Yury Stepanyants
Konferenz EGU General Assembly 2011
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 13 (2011)
Datensatznummer 250048045
 
Zusammenfassung
The extended Ostrovsky equation, (ut + cux + αuux + α1u2ux + βuxxx)x = γu, is used as a model of large-amplitude internal oceanic waves affected by Earth’s rotation. It contains two types of dispersion, the Boussinesq dispersion (~β), which accounts for non-hydrostatic effects and Coriolis dispersion (~γ) which accounts for the Earth’ rotation. In addition to that, the equation contains two nonlinear terms, quadratic (~α) and cubic (~α1) ones. The reduced version of the equation, that does not contain the small-scale Boussinesq dispersion, (ut + cux + αuux + α1u2ux)x = γu, is relevant for the description of very long internal waves when the non-hydrostatic effects are negligible. Such equation may be also of interest for description nonlinear waves of other physical origin in nonlinear media. In this paper we present a systematic analysis and categorization of stationary solutions to this extended reduced Ostrovsky equation. Periodic and solitary solutions are constructed and their typical parameters are estimated for the natural oceanic conditions.