On the use of a two-layer fluid stratification model in studies of topographically-generated baroclinic tides

V. I. Vlasenko; Nataliya Stashchuk

doi:10.1007/BF02346078

On the use of a two-layer fluid stratification model in studies of topographically-generated baroclinic tides

V. I. Vlasenko^*, Nataliya Stashchuk

^*Corresponding author for this work

School of Biological and Marine Sciences

Research output: Contribution to journal › Article › peer-review

Abstract

Internal waves generated by a baroclinic internal wave impinging on an oceanic ridge are studied. Two stratification models are considered: a two-layer ocean model (with a density jump) and a continuously stratified ocean model (model pycnocline). The results yielded by different stratification models are compared analytically. The analysis makes possible the application of a piecewise-constant approximation of the fluid stratification to study topographically-generated baroclinic tides.

Original language	English
Pages (from-to)	263-268
Number of pages	6
Journal	Soviet Journal of Physical Oceanography
Volume	2
Issue number	4
DOIs	https://doi.org/10.1007/BF02346078
Publication status	Published - Jul 1991

ASJC Scopus subject areas

Oceanography
Water Science and Technology
Ocean Engineering
General Environmental Science
Fluid Flow and Transfer Processes
General Earth and Planetary Sciences

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10.1007/BF02346078

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title = "On the use of a two-layer fluid stratification model in studies of topographically-generated baroclinic tides",

abstract = "Internal waves generated by a baroclinic internal wave impinging on an oceanic ridge are studied. Two stratification models are considered: a two-layer ocean model (with a density jump) and a continuously stratified ocean model (model pycnocline). The results yielded by different stratification models are compared analytically. The analysis makes possible the application of a piecewise-constant approximation of the fluid stratification to study topographically-generated baroclinic tides.",

author = "Vlasenko, {V. I.} and Nataliya Stashchuk",

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AB - Internal waves generated by a baroclinic internal wave impinging on an oceanic ridge are studied. Two stratification models are considered: a two-layer ocean model (with a density jump) and a continuously stratified ocean model (model pycnocline). The results yielded by different stratification models are compared analytically. The analysis makes possible the application of a piecewise-constant approximation of the fluid stratification to study topographically-generated baroclinic tides.

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On the use of a two-layer fluid stratification model in studies of topographically-generated baroclinic tides

Abstract

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