1992
DOI: 10.1016/0924-7963(92)90008-v
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On the wind-driven coastal upwelling in the Gulf of Lions

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Cited by 37 publications
(21 citation statements)
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“…The westward drift of the maturing food chain may favour higher trophic level organisms, suitable to sperm whale feeding, in the Gulf of Lions. Furthermore, northwesterly wind gales are common in the Gulf of Lions, even during summer, which generate coastal upwelling in this area (Hua & Thomasset 1983, Johns et al 1992, as well as vertical mixing linked to the complex canyon topography. Hence, several factors might contribute to high sperm whale abundance in this part of the western basin.…”
Section: Regional Variation In Sperm Whale Relative Abundancementioning
confidence: 99%
“…The westward drift of the maturing food chain may favour higher trophic level organisms, suitable to sperm whale feeding, in the Gulf of Lions. Furthermore, northwesterly wind gales are common in the Gulf of Lions, even during summer, which generate coastal upwelling in this area (Hua & Thomasset 1983, Johns et al 1992, as well as vertical mixing linked to the complex canyon topography. Hence, several factors might contribute to high sperm whale abundance in this part of the western basin.…”
Section: Regional Variation In Sperm Whale Relative Abundancementioning
confidence: 99%
“…Estournel et al (2003) showed that the wind stress curl, associated with Tramontane and Mistral, could explain the meso-scale eddy currents developing over the whole shelf. The possible suddenness and strength of these winds are likely to cause strong inertial oscillations of the current (Petrenko et al, 2005) and coastal upwelling, preferentially developing along rectilinear sections of the coast (Johns et al, 1992). In winter, these winds, rather dry and cold, extract a large amount of heat from the water column.…”
Section: Previous Applications Of Hydrodynamic Modeling In the North mentioning
confidence: 99%
“…This mesoscale activity is observed during the whole year by satellite imagery, although more eddies are observed during the winter (Hu et al 2009). After wind bursts, the NC can penetrate over the shelf: its variability, as well as the meanders and eddies that are associated with this current are responsible for a large part of the exchanges between the open ocean and the coastal waters (Albérola et al 1995, Estournel et al 2003, Johns et al 1992.…”
Section: Introductionmentioning
confidence: 99%
“…Numerous physical processes characterize the ocean circulation in the GoL, such as coastal up-and downwellings (Millot 1979, Johns et al 1992, winter dense water forming and cascading down the shelf break (Béthoux et al 2002, Dufau-Julliand et al 2004, local shelf circulation patterns (Estournel et al 2003, Petrenko et al 2005) and inertial and diurnal motions (Millot et al 1981).…”
Section: Introductionmentioning
confidence: 99%