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Abstract
Hydrographic and nephelometric data were gathered in the vicinity of the Grand-Rhoˆne canyon on the Golfe du Lion continental margin. These are used to describe the hydrographic structures and the suspended matter distribution. The results highlight the influence of wind-forced processes and current-canyon interaction on the dynamics in the canyon. These processes control the shelf-slope suspended matter exchanges, which are characterized by cross-canyon advection and near-bottom transfer along the axis of the canyon.
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