References of "Nihoul, Jacques"
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See detailGeneral summer circulation in the Northern Bering Sea.
Djenidi, Salim ULg; Deleersnijder, Eric; Nihoul, Jacques ULg

in EOS : Transactions, American Geophysical Union (1987), 68(50), 1719

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See detailPerspective in three-dimensional modelling of the marine system
Nihoul, Jacques ULg; Djenidi, Salim ULg

in Nihoul, J. C. J.; Jamart, B. M. (Eds.) Three-dimensional Models of Marine and Estuarine Dynamics (1987)

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See detailThe Modem contribution to Medalpex
Djenidi, Salim ULg; Nihoul, Jacques ULg; Clément, Francis et al

in Annales Geophysicae. Series B, Terrestrial and Planetary Physics (1987), 5B(1), 3-12

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See detailHydrodynamic models of the West European Shelf
Djenidi, Salim ULg; Nihoul, Jacques ULg; Ronday, François ULg

in Phys. of Shallow Bays, Estuaries and Cont. Shelves (1986)

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See detailThree-dimensional mathematical models for "marine weather" prediction
Nihoul, Jacques ULg; Djenidi, Salim ULg

in Zannetti (Ed.) Envirosoft 86 (1986)

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See detailModèles mathématiques de courants résiduels sur le plateau continental Nord Européen
Djenidi, Salim ULg; Nihoul, Jacques ULg; Ronday, François ULg et al

in Cabioch, Louis (Ed.) La Baie de Seine (1986)

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See detailA 3D numerical model of the Northern Bering Sea
Nihoul, Jacques ULg; Waleffe, Fabian; Djenidi, Salim ULg

in Environmental Software (1986), 2

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See detailEcohydrodynamical study of the Liguro-Proven Front (Corsica) I. Hydrological data
Hecq, Jean-Henri ULg; Licot, M.; Goffart, Anne ULg et al

in Van Grieken, R.; Wollast, R. (Eds.) Proceedings of the Symposium on Progress in Belgian Oceanography, Brussels, March 1985 (1985)

Hydrological measurements (temperature, conductivity, salinity) have been realized in 1982 and 1984 along the Calvi - Nice axis from the Corsican coast to 30 miles offshore. The data have shown a ... [more ▼]

Hydrological measurements (temperature, conductivity, salinity) have been realized in 1982 and 1984 along the Calvi - Nice axis from the Corsican coast to 30 miles offshore. The data have shown a thermohaline front separating low saline coastal waters of atlantic origin from high saline offshore waters of deeper origin. A succession of divergences and convergences is associated to that discontinuity. During spring, the front is emphasized and the water upwellings reach the surface. During summer, the upwellings are limited by the vertical stratification but an isopycnal inclination is always observed from the front to the coast. [less ▲]

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See detailEtudes d'impact d'aménagements sur le littoral corse
Lejeune, André ULg; Djenidi, Salim ULg; Sahloul, M. et al

in L'Hydraulique et la Maîtrise du Littoral (1984)

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