Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
1901319 | Wave Motion | 2009 | 11 Pages |
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.
Keywords
Related Topics
Physical Sciences and Engineering
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Geology
Authors
R.S. Johnson,