Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/49096
Title: External forcings, oceanographic processes and particle flux dynamics in Cap de Creus submarine canyon, NW Mediterranean Sea
Author: Rumín Caparrós, Aitor
Sànchez Vidal, Anna
Calafat Frau, Antoni
Canals Artigas, Miquel
Martín, Jacobo
Puig, Pere
Pedrosa-Pàmies, Rut
Keywords: Transport de sediments
Creus, Cap de (Catalunya)
Sediment transport
Creus, Cape (Catalonia)
Issue Date: 3-Jun-2013
Publisher: European Geosciences Union
Abstract: Particle fluxes (including major components and grain size), and oceanographic parameters (near-bottom water temperature, current speed and suspended sediment concentration) were measured along the Cap de Creus submarine canyon in the Gulf of Lions (GoL; NW Mediterranean Sea) during two consecutive winter-spring periods (2009 2010 and 2010 2011). The comparison of data obtained with the measurements of meteorological and hydrological parameters (wind speed, turbulent heat flux, river discharge) have shown the important role of atmospheric forcings in transporting particulate matter through the submarine canyon and towards the deep sea. Indeed, atmospheric forcing during 2009 2010 and 2010 2011 winter months showed differences in both intensity and persistence that led to distinct oceanographic responses. Persistent dry northern winds caused strong heat losses (14.2 × 103 W m−2) in winter 2009 2010 that triggered a pronounced sea surface cooling compared to winter 2010 2011 (1.6 × 103 W m−2 lower). As a consequence, a large volume of dense shelf water formed in winter 2009 2010, which cascaded at high speed (up to ∼1 m s−1) down Cap de Creus Canyon as measured by a current-meter in the head of the canyon. The lower heat losses recorded in winter 2010 2011, together with an increased river discharge, resulted in lowered density waters over the shelf, thus preventing the formation and downslope transport of dense shelf water. High total mass fluxes (up to 84.9 g m−2 d−1) recorded in winter-spring 2009 2010 indicate that dense shelf water cascading resuspended and transported sediments at least down to the middle canyon. Sediment fluxes were lower (28.9 g m−2 d−1) under the quieter conditions of winter 2010 2011. The dominance of the lithogenic fraction in mass fluxes during the two winter-spring periods points to a resuspension origin for most of the particles transported down canyon. The variability in organic matter and opal contents relates to seasonally controlled inputs associated with the plankton spring bloom during March and April of both years.
Note: Reproducció del document publicat a: http://dx.doi.org/10.5194/bg-10-3493-2013
It is part of: Biogeosciences, 2013, vol. 10, num. 6, p. 3493-3505
Related resource: http://dx.doi.org/10.5194/bg-10-3493-2013
URI: http://hdl.handle.net/2445/49096
ISSN: 1726-4170
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)
Publicacions de projectes de recerca finançats per la UE

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