Dependence of the dispersion curves on internal waves of a stratified ocean on the Vaisala-Brent frequency
Under the condition that the minimum of the Vaisala-Brent frequency (VBF) is greater than the Coriolis parameter, a parametric form of the dispersion curves of the internal gravitational waves in an ocean of constant depth with continuously variable VBF is obtained. This form is used when obtaining estimates of the dc displacements as a function of the VBF displacement and when isolating the VBF which admit of a unique restoration from a sequence of dispersion curves.
scientific article; zbMATH DE number 4024984