English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/113134
logo share SHARE   Add this article to your Mendeley library MendeleyBASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:

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

AuthorsSalat, Jordi ; Emelianov, Mikhail ; Fraile-Nuez, E.; Latasa, Mikel
Issue Date2013
PublisherInternational Commission for the Scientific Exploration of the Mediterranean Sea
CitationRapports 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)
AbstractOceanographic 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
Description40th CIESM Congress: The largest Forum on Mediterranean and Black Sea Research, 28 October - 1 November 2013, Marseille, France.-- 1 page, 2 figures
Publisher version (URL)http://ciesm.org/online/archives/abstracts/pdf/40/
Identifiersissn: 0373-434X
Appears in Collections:(ICM) Artículos
Files in This Item:
There are no files associated with this item.
Show full item record

WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.