Coupling coefficients and kinetic equation for Rossby waves in multi-layer ocean

The kinetic description of baroclinic Rossby waves in multi-layer model ocean is analysed. Explicit analytical expressions for the coupling coefficients describing energy exchange intensity between different modes are obtained and their main properties are established for the three-layer model....

Full description

Bibliographic Details
Main Author: T. Soomere
Format: Article
Language:English
Published: Copernicus Publications 2003-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/10/385/2003/npg-10-385-2003.pdf
_version_ 1818875268200136704
author T. Soomere
author_facet T. Soomere
author_sort T. Soomere
collection DOAJ
description The kinetic description of baroclinic Rossby waves in multi-layer model ocean is analysed. Explicit analytical expressions for the coupling coefficients describing energy exchange intensity between different modes are obtained and their main properties are established for the three-layer model. It is demonstrated that several types of interactions vanish in the case of simple vertical structures of the ocean, e.g. when all layers have equal depth. These cases correspond to a zero component of the eigenvectors of the potential vorticity equations. The kinetic equation always possesses a fully barotropic solution. If energy is concentrated in the baroclinic modes, the barotropic mode will necessarily be generated. Motion systems consisting of a superposition of the barotropic and a baroclinic mode always transfer energy to other baroclinic modes.
first_indexed 2024-12-19T13:23:48Z
format Article
id doaj.art-583688cedeca438c9615b67aac01fb0c
institution Directory Open Access Journal
issn 1023-5809
1607-7946
language English
last_indexed 2024-12-19T13:23:48Z
publishDate 2003-01-01
publisher Copernicus Publications
record_format Article
series Nonlinear Processes in Geophysics
spelling doaj.art-583688cedeca438c9615b67aac01fb0c2022-12-21T20:19:38ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462003-01-01104/5385396Coupling coefficients and kinetic equation for Rossby waves in multi-layer oceanT. SoomereThe kinetic description of baroclinic Rossby waves in multi-layer model ocean is analysed. Explicit analytical expressions for the coupling coefficients describing energy exchange intensity between different modes are obtained and their main properties are established for the three-layer model. It is demonstrated that several types of interactions vanish in the case of simple vertical structures of the ocean, e.g. when all layers have equal depth. These cases correspond to a zero component of the eigenvectors of the potential vorticity equations. The kinetic equation always possesses a fully barotropic solution. If energy is concentrated in the baroclinic modes, the barotropic mode will necessarily be generated. Motion systems consisting of a superposition of the barotropic and a baroclinic mode always transfer energy to other baroclinic modes.http://www.nonlin-processes-geophys.net/10/385/2003/npg-10-385-2003.pdf
spellingShingle T. Soomere
Coupling coefficients and kinetic equation for Rossby waves in multi-layer ocean
Nonlinear Processes in Geophysics
title Coupling coefficients and kinetic equation for Rossby waves in multi-layer ocean
title_full Coupling coefficients and kinetic equation for Rossby waves in multi-layer ocean
title_fullStr Coupling coefficients and kinetic equation for Rossby waves in multi-layer ocean
title_full_unstemmed Coupling coefficients and kinetic equation for Rossby waves in multi-layer ocean
title_short Coupling coefficients and kinetic equation for Rossby waves in multi-layer ocean
title_sort coupling coefficients and kinetic equation for rossby waves in multi layer ocean
url http://www.nonlin-processes-geophys.net/10/385/2003/npg-10-385-2003.pdf
work_keys_str_mv AT tsoomere couplingcoefficientsandkineticequationforrossbywavesinmultilayerocean