{"title":"Hydrodynamique de l’estuaire de la lagune Ebrié (Côte d'Ivoire)","authors":"S. Monde, A. Coulibaly, Ted-Edgard Wango, K. Aka","doi":"10.5150/REVUE-PARALIA.2011.001","DOIUrl":null,"url":null,"abstract":"Les baies estuariennes d’Abidjan subissent une forte pression anthropique qui modifie la circulation des masses d’eaux. En outre, ces baies presentent des signes de pollution. Afin de mieux cerner les processus qui s’y deroulent des approches morphobathymetrique et dynamique ont ete mise en œuvre. Il en ressort que les baies estuariennes presentent des morphologies symetriques par rapport a l'axe central de la lagune Ebrie. Dans les chenaux etroits, les courants sont exclusivement alternatifs. Les vitesses des courants dans les baies de Cocody et de Bietri sont decrites. Les evolutions du niveau de l’eau, de la salinite et de la temperature sont etudiees dans la lagune sur 200 jours. Les variations de salinite dans la lagune s’agencent dans les saisons continentale et marine et dependent des fortes precipitations et des crues fluviales. Il en est de meme pour l’evolution de la temperature des eaux qui varie en fonction des precipitations et des debits fluviaux. Translated version: Hydrodynamics of the estuary of the lagoon Ebrie (Cote d'Ivoire) The estuarine bays of Abidjan are under severe anthropogenic pressure which alters the movement of water masses. In addition, these bays are showing signs of pollution. To better understand the processes that take place, morphobathymetric and dynamic approaches have been implemented. It appears that the morphology of estuarine bays is symmetrical about the central axis of the Ebrie lagoon. In narrow channels, the currents are only alternative. Current velocities in Cocody and Bietri Bays are described. The time evolution of water surface level, salinity and temperature are studied in the lagoon over days. Variations in salinity in the lagoon are related to continental and marine seasons and depend on heavy rains and river floods. It is the same for changes in water temperatures that vary according to rainfall and river flows. Keywords: Bay; Estuary; Morphobathymetry; Hydrodynamics; Ebrie Lagoon.","PeriodicalId":202784,"journal":{"name":"Revue Paralia","volume":"48 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2011-02-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Revue Paralia","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5150/REVUE-PARALIA.2011.001","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 2
Abstract
Les baies estuariennes d’Abidjan subissent une forte pression anthropique qui modifie la circulation des masses d’eaux. En outre, ces baies presentent des signes de pollution. Afin de mieux cerner les processus qui s’y deroulent des approches morphobathymetrique et dynamique ont ete mise en œuvre. Il en ressort que les baies estuariennes presentent des morphologies symetriques par rapport a l'axe central de la lagune Ebrie. Dans les chenaux etroits, les courants sont exclusivement alternatifs. Les vitesses des courants dans les baies de Cocody et de Bietri sont decrites. Les evolutions du niveau de l’eau, de la salinite et de la temperature sont etudiees dans la lagune sur 200 jours. Les variations de salinite dans la lagune s’agencent dans les saisons continentale et marine et dependent des fortes precipitations et des crues fluviales. Il en est de meme pour l’evolution de la temperature des eaux qui varie en fonction des precipitations et des debits fluviaux. Translated version: Hydrodynamics of the estuary of the lagoon Ebrie (Cote d'Ivoire) The estuarine bays of Abidjan are under severe anthropogenic pressure which alters the movement of water masses. In addition, these bays are showing signs of pollution. To better understand the processes that take place, morphobathymetric and dynamic approaches have been implemented. It appears that the morphology of estuarine bays is symmetrical about the central axis of the Ebrie lagoon. In narrow channels, the currents are only alternative. Current velocities in Cocody and Bietri Bays are described. The time evolution of water surface level, salinity and temperature are studied in the lagoon over days. Variations in salinity in the lagoon are related to continental and marine seasons and depend on heavy rains and river floods. It is the same for changes in water temperatures that vary according to rainfall and river flows. Keywords: Bay; Estuary; Morphobathymetry; Hydrodynamics; Ebrie Lagoon.