Occurrence of a subsurface anticyclonic eddy, fronts, and Trichodesmium spp.

Occurrence of a subsurface anticyclonic eddy, fronts, and Trichodesmium spp.

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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Auteurs principaux: Aldeco-Ramírez, J, Monreal-Gómez, MA, Signoret, M, Salas-de-León, DA, Hernández-Becerril, DU
Format: info:eu-repo/semantics/article
Langue:eng
Publié: Iniversidad Autónoma de Baja California 2009
Sujets:
anticyclonic eddy
fronts
Trichodesmium
Campeche Canyon
Gulf of Mexico
Accès en ligne:https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/1551
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https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/1551

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