| dc.contributor.author | Brink, Kenneth H. | | |
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| dc.date.accessioned | 2012-04-23T17:50:41Z | | | |
| dc.date.available | 2012-04-23T17:50:41Z | | | |
| dc.date.issued | 2011-07-01 | | | |
| dc.identifier.citation | Journal of Marine Research 69 (2011): 483-499 | en_US | | |
| dc.identifier.uri | https://hdl.handle.net/1912/5139 | | | |
| dc.description | Author Posting. © Sears Foundation for Marine Research, 2011. This article is posted here by permission of Sears Foundation for Marine Research for personal use, not for redistribution. The definitive version was published in Journal of Marine Research 69 (2011): 483-499, doi:10.1357/002224011799849354. | en_US | | |
| dc.description.abstract | Mean flow generation by oscillating currents is considered in an idealized stratified ocean with a corrugated shelf-slope topography. Numerical model results for near-bottom mean along-isobath flow show a general parameter dependence similar to that found with no stratification (Brink, 2010). Stratification, however, makes the interior rectified flow depth-dependent, and usually bottom-intensified. Scalings for both the mean flow and its vertical dependence are developed and evaluated. Two crude comparisons against observed mean oceanic flows suggest that the present results may parameterize the mean flow magnitude correctly. | en_US | | |
| dc.description.sponsorship | Thisworkwas sponsored by the Physical Oceanography Program at the National
Science Foundation through grant OCE-0751731. | en_US | | |
| dc.format.mimetype | application/pdf | | | |
| dc.language.iso | en_US | en_US | | |
| dc.publisher | Sears Foundation for Marine Research | en_US | | |
| dc.relation.uri | https://doi.org/10.1357/002224011799849354 | | | |
| dc.title | Topographic rectification in a stratified ocean | en_US | | |
| dc.type | Article | en_US | | |
| dc.identifier.doi | 10.1357/002224011799849354 | | | |
