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Provedor de dados:  ArchiMer
País:  France
Título:  Le "fleuve cotier": Un phenomene hydrologique important en Manche orientale. Exemple du Pas-de-Calais
Autores:  Brylinski, J M
Lagadeuc, Y
Gentilhomme, V
Dupont, J P
Lafite, R
Dupeuble, P A
Huault, M F
Auger, Y
Data:  1991
Ano:  1991
Resumo:  The English Channel has a "megatidal" regime: in the Dover Strait, the tidal range varies between 3 and 9 m in neap-tide and spring-tide respectively. The tide currents are alternating and essentially parallel to the coast. Along the French coast, the fluvial supplies, distributed from the Bay of Seine to Cape Gris-Nez, generate a coastal water mass which drifts nearshore, separated from the open sea by a frontal area: this coastal flow is characterized by its freshness, turbidity, phytoplankton richness, and pollution content. Its width is only 3 to 5 miles, but because of the high concentrations of dissolved and suspended components, it is possible that the coastal flow plays an important role in the fluxes between the Eastern Channel and the North Sea.
Tipo:  Text
Idioma:  Francês
Editor:  Gauthier-Villars
Formato:  application/pdf
Fonte:  Oceanologica Acta, Special issue (0399-1784) (Gauthier-Villars), 1991
Direitos:  info:eu-repo/semantics/openAccess

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