Occurrence of a subsurface anticyclonic eddy, fronts, and Trichodesmium spp. over the Campeche Canyon region, Gulf of Mexico
Eddies and fronts created by geostrophic balance between counter-rotating currents are hydrodynamic processes that concentrate or dilute plankton and suspended material by physical processes of accumulation, retention, or dispersion. Over Campeche Canyon, in the southern Gulf of Mexico, observations...
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| Pubblicato in: | Ciencias Marinas |
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| Autori principali: | , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
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Universidad Autónoma de Baja California
2009
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| Soggetti: | |
| Accesso online: | https://www.redalyc.org/articulo.oa?id=48013184002 |
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