Open AccessThree‐dimensional shoaling of large‐amplitude internal waves
Author(s) -
Vlasenko V.,
Stashchuk N.
Publication year - 2007
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2007jc004107
Subject(s) - shoaling and schooling , geology , refraction , amplitude , wave shoaling , internal wave , breaking wave , curvature , waves and shallow water , stratification (seeds) , geophysics , gravity wave , surface wave , turbulence , physics , mechanics , wave propagation , mechanical wave , optics , longitudinal wave , geometry , oceanography , seed dormancy , mathematics , germination , botany , dormancy , biology
The three‐dimensional (3‐D) shoaling of large‐amplitude internal waves (LAIW) is studied in the framework of a fully nonlinear nonhydrostatic numerical model. The vertical fluid stratification, parameters of the propagating waves and bottom topography were taken close to those observed in the northern part of the Andaman Sea. It was found that three‐dimensional evolution of LAIWs propagating from the deep part of a basin onto the shelf differs from two‐dimensional shoaling in many ways largely because of the process of wave refraction developing in the areas of local bottom elevations or depressions. In the 3‐D case the wave refraction produces concave and convex fragments of the wave fronts which may lead to the transverse redistribution of energy along the wave. Results demonstrate that concave wave fragments work as optical lenses focusing the wave energy to the centers of curvature. This process is especially important for LAIWs in shallow water zones where wave amplitudes are close to the saturation level. In general, the wave refraction leads to more fast wave breaking than that in the 2‐D case. As a results, it should be expected to find localized regions of higher levels of water mixing and turbulence in the vicinity of local banks and headlands where LAIWs produce concave patterns. The areas of local bottom depressions, on the contrary, should be considered as potential places with lower level of background mixing.