The exchange of fluid mass between quasi-geostrophic and ageostrophic motions during the reflection of Rossby waves from a coast. I. The case of an infinite rectilinear coast-Reference-Cited by-同舟云学术

The exchange of fluid mass between quasi-geostrophic and ageostrophic motions during the reflection of Rossby waves from a coast. I. The case of an infinite rectilinear coast

Published:1992-01 Issue:3-4 Volume:16 Page:305-329
ISSN:0377-0265
Container-title:Dynamics of Atmospheres and Oceans
language:en
Short-container-title:Dynamics of Atmospheres and Oceans

Author:

Dorofeyev Victor L.,Larichev Vitaly D.

Publisher

Elsevier BV

Subject

Atmospheric Science,Computers in Earth Sciences,Geology,Oceanography

Reference15 articles.

1. Long period divergent planetary waves;Buchwald;Geophys. Fluid Dyn.,1973

2. Numerical modelling of interaction of Rossby solitons with coastal boundaries;Dorofeyev;Mar. Hydrophys. Res.,1988

3. Simple applications of McWilliams' ‘A note on a consistent quasigeostrophic model in a multiply connected domain’;Flierl;Dyn. Atmos. Oceans,1977

4. Ageostrophic effects in rotating stratified flow;Huppert;J. Fluid Mech.,1974

5. Internal Kelvin waves generated by quasi-periodic mesoscale motion along the coast;Ikeda;J. Phys. Oceanogr.,1985

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