English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/110015
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:


Hydrodynamics over the Gulf of Valencia continental slope and their role in sediment transport

AuthorsRibó, Marta ; Puig, Pere ; van Haren, H.
KeywordsWestern Mediterranean
Sediment transport
Continental slope
Gulf of Valencia
Issue DateJan-2015
PublisherPergamon Press
CitationDeep-Sea Research Part I: Oceanographic Research Papers 95: 54-66 (2015)
AbstractCirculation patterns and sediment dynamics were studied over the Gulf of Valencia (GoV) continental slope during spring and winter 2011-2012. Two moorings were deployed at two locations; at 450m depth from February to May 2011, and at 572m depth from October 2011 to February 2012. At both mooring sites, observations were made of currents, temperature and near-bottom turbidity within the lowermost 80m above the seafloor. The temperature measurements allowed distinction of the different water masses and their temporal evolution. The fluctuations of the boundary between the Western Mediterranean Deep Water (WMDW) and the Levantine Intermediate Water (LIW) masses were monitored, and several intrusions of Western Mediterranean Intermediate Water (WIW) were observed, generally coinciding with changes in current direction. At both mooring sites, the currents generally maintained low velocities <10cms-1, with several pulses of magnitude increases >20cms-1, and few reaching up to 35cm s-1, associated with mesoscale eddies and topographic waves. The current direction was mainly towards the SSE on the first deployment and to the ESE on the second deployment. This second location was affected by a strong bottom offshore veering presumably generated by local topographic effects. Increases in suspended sediment concentrations (SSC) were observed repeatedly throughout the records, reaching values >3mgl-1. However, these SSC variations were uncorrelated with changes in velocity magnitude and direction and/or with temperature oscillations. Results presented in this paper highlight the complex relation between the hydrodynamics and sediment transport over the GoV continental slope, and suggest that other potential sediment resuspension mechanism not linked with current fluctuations, might play a key role in the present-day sedimentary dynamics. Resuspension due to bottom trawling appears to be the most plausible mechanism. © 2014 Elsevier Ltd.
Description13 pages, 13 figures
Publisher version (URL)http://dx.doi.org/10.1016/j.dsr.2014.10.004
Identifiersdoi: 10.1016/j.dsr.2014.10.004
issn: 0967-0637
e-issn: 1879-0119
Appears in Collections:(ICM) Artículos
Files in This Item:
There are no files associated with this item.
Show full item record
Review this work

Related articles:

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