AUTHORS: Oxana Kurkina, Ekaterina Rouvinskaya, Andrey Kurkin, Lidiya Talalushkina, Ayrat Giniyatullin
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ABSTRACT: The structure of the velocity field induced by internal solitary waves of the first and second modes is determined. The contribution from second-order terms in asymptotic expansion into the horizontal velocity is estimated for the models of almost two- and three-layer fluid density stratification for solitons of positive and negative polarity. The influence of the nonlinear correction manifests itself firstly in the shape of the lines of zero horizontal velocity: they are curved and the shape depends on the soliton amplitude and polarity while for the leading-order wave field they are horizontal. Also the wave field accounting for the nonlinear correction for mode I waves has smaller maximal absolute values of negative velocities (near-surface for the soliton of elevation, and near-bottom for the soliton of depression) and larger maximums of positive velocities. Thus for the solitary internal waves of positive polarity weakly nonlinear theory overestimates the near-bottom velocities and underestimates the near-surface current. For solitary waves of negative polarity, which are the most typical for hydrological conditions of low and middle latitudes, the situation is the opposite. II mode soliton’s velocity field in almost two-layer fluid reaches its maximal absolute values in a middle layer instead of near-bottom and near-surface maximums for I mode solitons.
KEYWORDS: Internal waves, Gardner equation, near-bottom velocity, near-surface velocity
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