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dc.contributor.authorDurrieu de Madron, Xavier-
dc.contributor.authorPuig, Pere-
dc.contributor.authorFont, Jordi-
dc.contributor.authorMartín, Jacobo-
dc.contributor.authorPalanques, Albert-
dc.identifiere-issn: 1607-7962-
dc.identifier.citationGeophysical Research Abstracts 15: EGU2013-10889-1 (2013)-
dc.descriptionDurrieu de Madron, Xavier ... et al.-- European Geosciences Union General Assembly 2013, 7-12 April, Vienna, Austria-
dc.description.abstractThe winter of 2012 experienced peculiar atmospheric conditions that triggered a massive formation of dense water on the continental shelf and in the deep basin of the Gulf of Lions. Multi-platforms observations enabled, with an unprecedented resolution, a synoptic view of dense water formation and spreading at basin scale. Five months after its formation, the dense water of coastal origin created a distinct bottom layer up to few hundreds of meters thick over the central part of the NW Mediterranean basin, which was overlaid by a layer of newly formed deep water produced by open-sea convection. These observations highlight the role of intense episodes of both dense shelf water cascading and open-sea convection to the alteration of the characteristics of the NW Mediterranean deep waters-
dc.publisherEuropean Geosciences Union-
dc.titleInteraction of dense dense shelf water cascading and open-sea convection in the Northwestern Mediterranean during winter 2012-
dc.typepóster de congreso-
dc.description.versionPeer Reviewed-
Appears in Collections:(ICM) Comunicaciones congresos
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