Effects of extreme meteorological conditions on coastal dynamics near a submarine canyon
Effects of extreme meteorological conditions on coastal dynamics near a submarine canyon
A 3-D hydrodynamic model is applied to assess shelf/slope exchanges in the Calvi Canyon region (Corsica, NW Mediterranean) during the violent storm that affected the Western Europe in December 1999. Simulations are carried out using high-frequency sampling meteorological data to take into account the short-term variability of the atmospheric conditions. It is shown that the combined effects of canyon topography and of the wind forcing during the storm are responsible for a large increase of both cross-shore and vertical transports in the area. Strong downwelling motion is simulated all along the continental slope with vertical velocities up to 2 cm s?1 within the canyon. High turbulent diffusion levels are obtained leading to the complete mixing of the water column within the canyon. Results suggest that increased turbulent diffusion and downwelling circulation in the canyon during the storm should result in a large transport of coastal water towards the abyssal plain.
Submarine canyons, Shelf edge dynamics, Downwelling, Modelling, Mediterranean Sea, Corsica
1033-1045
Skliris, N.
07af7484-2e14-49aa-9cd3-1979ea9b064e
Lacroix, G.
395fbf23-57a3-4f71-bf3e-8a6b77b56a34
Djenidi, S.
0c0f008b-5712-4d8e-aa58-d10ccf3a57b1
June 2004
Skliris, N.
07af7484-2e14-49aa-9cd3-1979ea9b064e
Lacroix, G.
395fbf23-57a3-4f71-bf3e-8a6b77b56a34
Djenidi, S.
0c0f008b-5712-4d8e-aa58-d10ccf3a57b1
Skliris, N., Lacroix, G. and Djenidi, S.
(2004)
Effects of extreme meteorological conditions on coastal dynamics near a submarine canyon.
Continental Shelf Research, 24 (9), .
(doi:10.1016/j.csr.2004.02.012).
Abstract
A 3-D hydrodynamic model is applied to assess shelf/slope exchanges in the Calvi Canyon region (Corsica, NW Mediterranean) during the violent storm that affected the Western Europe in December 1999. Simulations are carried out using high-frequency sampling meteorological data to take into account the short-term variability of the atmospheric conditions. It is shown that the combined effects of canyon topography and of the wind forcing during the storm are responsible for a large increase of both cross-shore and vertical transports in the area. Strong downwelling motion is simulated all along the continental slope with vertical velocities up to 2 cm s?1 within the canyon. High turbulent diffusion levels are obtained leading to the complete mixing of the water column within the canyon. Results suggest that increased turbulent diffusion and downwelling circulation in the canyon during the storm should result in a large transport of coastal water towards the abyssal plain.
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Published date: June 2004
Keywords:
Submarine canyons, Shelf edge dynamics, Downwelling, Modelling, Mediterranean Sea, Corsica
Organisations:
Physical Oceanography
Identifiers
Local EPrints ID: 365219
URI: http://eprints.soton.ac.uk/id/eprint/365219
ISSN: 0278-4343
PURE UUID: 9e560054-7b60-4a67-af1d-4b992579a843
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Date deposited: 28 May 2014 09:16
Last modified: 15 Mar 2024 03:39
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Author:
G. Lacroix
Author:
S. Djenidi
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