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Analysis of the variability of hydrological characteristics of the north subpolar front using the model of frontal-trapped baroclinic Rossby waves
Authors:K P Belyaev  S S Lappo  V P Tereshchenkov
Abstract:Solutions, termed frontal-trapped Rossby waves, have been found for the long-wave equation in a model of a two-layer fluid with the frontal boundary given in the form of an exponential function. Data from a hydrological survey of a subpolar hydrological front in the vicinity of Newfoundland are analysed. A frontal-trapped wave model is shown to describe about 40% of the dispersion of the initial seawater density field. Translated by V. Puchkin.
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