Classification of internal waves shoaling over slope-shelf topography
Presented by Kateryna Terletska
Abstract: The shoaling of an internal solitary waves of depression in two layer fluid with an idealized slope-shelf topography is studied to classify the regimes of shoaling. Two mechanisms were assumed to be essential during wave shoaling: (i) wave breaking resulting in mixing and (ii) changing of the polarity of the initial wave of depression over the slope into wave of elevation on the shelf. Proposed three-dimensional
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