Plankton transfers and coastal front in the dover strait

Type Article
Date 1993
Language English
Author(s) Brylinski Jm, Aelbrecht D
Affiliation(s) IMG,LEGI,URA 1509,F-38041 GRENOBLE,FRANCE
Meeting Channel Symposium on Fluxes and Processes within a Macrotidal Sea, BREST, FRANCE, SEP 02-04, 1992
Source Oceanologica Acta (0399-1784) (Gauthier-Villars), 1993 , Vol. 16 , N. 5-6 , P. 671-676
WOS© Times Cited 7
Keyword(s) ZOOPLANKTON, FRONT, VERTICAL MIGRATION, RECRUITMENT, ENGLISH CHANNEL
Abstract Zooplankton and current studies were carried out in the coastal front of the Dover Strait. We show that the maintenance of both offshore and inshore planktonic communities is due to two coupled phenomena: 1) the residual drift of water differs in the upper and in the deeper waters; and 2) the vertical distribution of plankton differs for inshore and offshore species. In the frontal area, the coastal species remain in the lower water layer where the residual drift is landward. Conversely, the offshore species remain in the upper water layer where the residual drift is seaward.
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