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Continental Shelf Research
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Continental Shelf Research
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Suspended sediment transport in the Gulf of Lions (NW Mediterranean): Impact of extreme storms and floods

Authors: Ulses, C.; Estournel, C.; Durrieu de Madron, Xavier; Palanques, A.;

Suspended sediment transport in the Gulf of Lions (NW Mediterranean): Impact of extreme storms and floods

Abstract

In situ observations were combined with 3D modeling to gain understanding of and to quantify the suspended sediment transport in the Gulf of Lions (NW Mediterranean Sea). The outputs of a hydrodynamic-sediment transport coupled model were compared to near-bottom current and suspended sediment concentration measurements collected at the head of seven submarine canyons and at a shallow shelf site, over a 6-month period (November 2003-May 2004). The comparisons provide a reasonable validation of the model that reproduces the observed spatial and time variations. The study period was marked by an unusual occurrence of marine storms and high river inputs. The major water and sediment discharges were supplied by the Rhone, the largest Mediterranean river, during an exceptional flood accompanying a severe marine storm in early December 2003. A second major storm, with moderate flooding, occurred in February 2004. The estimate of river input during the studied period was 5.9 Mt. Our study reveals (i) that most of the particulate matter delivered by the Rhone was entrapped on the prodelta, and (ii) that marine storms played a crucial role on the sediment dispersal on the shelf and the off-shelf export. The marine storms occurring in early December 2003 and late February 2004 resuspended a very large amount of shelf sediment (>8 Mt). Erosion was controlled by waves on the inner shelf and by energetic currents on the outer shelf. Sediment deposition took place in the middle part of the shelf, between 50 and 100 m depth. Resuspended sediments and river-borne particles were transported to the southwestern end of the shelf by a cyclonic circulation induced by these onshore winds and exported towards the Catalan shelf and into the Cap de Creus Canyon which incises the slope close to the shore. Export taking place mostly during marine storms was estimated to reach 9.1 Mt during the study period. © 2008 Elsevier Ltd. All rights reserved

This study was supported by the EUROSTRATAFORM Project funded by EU (EVK3-CT-2002-00079), within EU Fifth Framework Programme: Energy, Environment and Sustainable Development

Special issue Sediment Dynamics in the Gulf of Lions; the Impact of Extreme Events.-- 23 pages, 10 figures, 5 tables, 3 appendix

Peer Reviewed

Countries
Netherlands, France, France
Keywords

3D sediment transport modeling, Continental margins, Sediment transport, Sediment budget, [PHYS.PHYS.PHYS-AO-PH] Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph], [SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces, environment, Northwestern Mediterranean, Sediment resuspension, Gulf of Lions, Northwestern Mediterranean Sea

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selected citations
These citations are derived from selected sources.
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
views
OpenAIRE UsageCountsViews provided by UsageCounts
138
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Top 10%
38
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