Por favor, use este identificador para citar o enlazar a este item:
http://hdl.handle.net/10261/113134
COMPARTIR / EXPORTAR:
SHARE BASE | |
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE | |
Título: | After Deep Water formation: sinking and spreading or reorganising phase, including upwelling? |
Autor: | Salat, Jordi CSIC ORCID ; Emelianov, Mikhail CSIC ORCID ; Fraile-Nuez, Eugenio ; Latasa, Mikel CSIC ORCID | Fecha de publicación: | 2013 | Editor: | International Commission for the Scientific Exploration of the Mediterranean Sea | Citación: | Rapports 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) |
Resumen: | Oceanographic 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 | Descripción: | 40th CIESM Congress: The largest Forum on Mediterranean and Black Sea Research, 28 October - 1 November 2013, Marseille, France.-- 1 page, 2 figures | Versión del editor: | http://ciesm.org/online/archives/abstracts/pdf/40/ | URI: | http://hdl.handle.net/10261/113134 | Identificadores: | issn: 0373-434X |
Aparece en las colecciones: | (ICM) Informes y documentos de trabajo |
Mostrar el registro completo
CORE Recommender
NOTA: Los ítems de Digital.CSIC están protegidos por copyright, con todos los derechos reservados, a menos que se indique lo contrario.