| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4548436 | Journal of Marine Systems | 2011 | 11 Pages |
Abstract
⺠Sources of stratification can be quantified from field measurements at a site. ⺠Degrees of stratification can show an apparent response to residual circulation. ⺠Ekman veering can be substantial in shallow, stratified coastal waters. ⺠Stratification is the outcome of a delicate balance of counteracting processes. ⺠Density topography becomes complex when a buoyancy source is distributed.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Oceanography
Authors
A.J.F. Hoitink, D.S. van Maren, P. Hoekstra,