Abstract
Depth variations of the power spectrum of underwater turbulence are obtained. Considered specific medium is the Atlantic Ocean at mid and low latitudes. Associated temperature and salinity changes at low latitude, mid latitude–summer and mid latitude-winter are found for the Nikishovs’ spectrum model. By employing the equations for the temperature and salinity changes, figures for the rate of dissipation of the mean squared refractive index fluctuation, rate of dissipation of turbulent kinetic energy per unit mass of fluid and the relative strength of temperature and salinity fluctuations against the depth in underwater are provided. Additionally, plots of the power spectra of underwater turbulence are presented against the changes in the depth.
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