Article ID Journal Published Year Pages File Type
1901319 Wave Motion 2009 11 Pages PDF
Abstract
The case of large negative vorticity is then considered, and this does permit a solution that is close to stagnation, a conclusion consistent with the linear dispersion relation. No corresponding solution exists for large positive vorticity. Some typical streamlines and velocity profiles below the crest, based on the asymptotic results, are presented.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
Authors
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