Frontal subduction of a cool surface water mass in the Gulf of Tehuantepec, Mexico
The southward wind events in the Gulf of Tehuantepec generate large warm eddies and strong offshore current jets thatproduce entrainment of subsurface waters into the upper ocean resulting in cool (dense) water masses. Strong frontal featuresoccur at the boundary between warm eddies and cool patches...
Tallennettuna:
| Julkaisussa: | Geofísica Internacional |
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| Päätekijät: | , , , |
| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
Universidad Nacional Autónoma de México
2003
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| Aiheet: | |
| Linkit: | https://www.redalyc.org/articulo.oa?id=56842109 |
| Tagit: |
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