title: Method of Detecting the Long-Wave Structure of Sea Currents, Measured Only in One Point
abstract: It is shown within the framework of the semi-spectral linear model of wind-driven currents, that if temporal changes of the level inclination are mainly of a reverse character, that takes place in case of long-wave structure of gradient currents, then the similarity of their spectral tensors (the spectral tensor similarity criterion) does not depend on the level and bottom inclinations and is determined only in depth, by a vertical coordinate, viscosity, the angular frequency and the Coriolis pa
journal: Turkish Journal of Fisheries and Aquatic Sciences