作者: Eric Wolanski , Takashi Asaeda , Akihiro Tanaka , Eric Deleersnijder
DOI: 10.1016/0278-4343(95)00087-9
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摘要: Results of field, laboratory and numerical studies are used to describe the three-dimensional circulation in a barotropic island wake shallow waters. Bottom friction generates closed characterized by strong upwelling (typically 10-20 m h(-1)) bulk eddy an even larger downwelling velocity narrow zone along edges eddy. This exists at solid boundaries also all separation streamline. can be realistically modeled numerically provided intense turbulence free shear layers is explicitly parameterized. secondary aggregates buoyant material well-mixed coastal Copyright (C) 1996 Elsevier Science Ltd.