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Sibirskii Zhurnal Vychislitel'noi Matematiki, 2009, Volume 12, Number 4, Pages 449–463 (Mi sjvm139)  

On barotropic trapped wave solutions with no-slip boundary conditions

S. V. Smirnov

Institute for Automation and Control Processes, Far Eastern Branch of the Russian Academy of Sciences
References:
Abstract: Barotropic trapped wave solutions of a linearized system of the ocean dynamics equations are described, for semi-infinite, $f$-plane model basin of a constant depth bordering a straight, vertical coast, for some “typical” values of the model parameters. No-slip boundary conditions are considered. When the wave length is shorter than the Rossby deformation radius, the main features of the wave solutions are as follows: the Kelvin wave exponential offshore decay scale essentially decreases as the wave length decreases, an additional wave solution propagating in the opposite direction appears.
Key words: ocean dynamics, trapped waves, Kelvin wave.
Received: 30.01.2008
Revised: 24.03.2009
English version:
Numerical Analysis and Applications, 2009, Volume 2, Issue 4, Pages 364–376
DOI: https://doi.org/10.1134/S1995423909040089
Bibliographic databases:
UDC: 517.955.8+551.466
Language: Russian
Citation: S. V. Smirnov, “On barotropic trapped wave solutions with no-slip boundary conditions”, Sib. Zh. Vychisl. Mat., 12:4 (2009), 449–463; Num. Anal. Appl., 2:4 (2009), 364–376
Citation in format AMSBIB
\Bibitem{Smi09}
\by S.~V.~Smirnov
\paper On barotropic trapped wave solutions with no-slip boundary conditions
\jour Sib. Zh. Vychisl. Mat.
\yr 2009
\vol 12
\issue 4
\pages 449--463
\mathnet{http://mi.mathnet.ru/sjvm139}
\transl
\jour Num. Anal. Appl.
\yr 2009
\vol 2
\issue 4
\pages 364--376
\crossref{https://doi.org/10.1134/S1995423909040089}
\scopus{https://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-77952860260}
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