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Título

After Deep Water formation: sinking and spreading or reorganising phase, including upwelling?

AutorSalat, Jordi CSIC ORCID ; Emelianov, Mikhail CSIC ORCID ; Fraile-Nuez, Eugenio ; Latasa, Mikel CSIC ORCID
Fecha de publicación2013
EditorInternational Commission for the Scientific Exploration of the Mediterranean Sea
CitaciónRapports et procès verbaux des réunions - Commission internationale pour l'exploration scientifique de la mer Méditerranée 40: 175 (2013)
Rapport du 40e Congrès de la CIESM : 40th CIESM Congress Proceedings: 175 (2013)
ResumenOceanographic data obtained by mid spring at open sea in the central part of the NW Mediterranean reveal evidences that almost two months after the open sea Deep Water Formation (DWF) process, there are still energetic mechanisms reorganising the water mass structure. Among those, clear indications of a relevant upwelling below the thermocline, that would contribute to maintain the early spring open sea phytoplankton bloom
Descripción40th CIESM Congress: The largest Forum on Mediterranean and Black Sea Research, 28 October - 1 November 2013, Marseille, France.-- 1 page, 2 figures
Versión del editorhttp://ciesm.org/online/archives/abstracts/pdf/40/
URIhttp://hdl.handle.net/10261/113134
Identificadoresissn: 0373-434X
Aparece en las colecciones: (ICM) Informes y documentos de trabajo

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