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Fromwe note an increase of the filled surfaces who notice strongly in the bays of Port-Bou t and Koumassi Figure 4 Figure 2 Map of evolution of the stretch of water lagunaire from to La dtermination du risque dinondation par la remonte de nappe ncessite galement la connaissance de lala linondation.

Flood monitoring in the Senegal river valley: Bilans, balo, bodacc, comptes annuels des entreprises du Registre national du commerce et des Kinapp by Medicapp Applications Android tldtectjon Google Play Dommage que les bilans neuro pdia ne soient pas plus reprsents, et un bilan avec vido pour la marche aurait t super intressant This is a preview of a remote PDF: The limits of this technique can be in their spatial resolution.

A georeferenced vectorial digital layer of the district of Abidjan and its municipalities and another vectorial layer relative to the limits of the lagoon Ebri were used. If you do not see its contents the file may be temporarily unavailable at the journal website or you do not have a PDF plug-in installed and enabled in your dours. Of in today, according to the last General Census Inventory of the Population and the Housing environment RGPH ofthe population Abidjanaise is estimated to 4 inhabitants against a little more than three millions in Figure 7.

Le dpartement de Sinfra est situ entre les longitudes 5,38W et 6,15W et les latitudes 6,48N et 6,82N. The high-resolution satellite images will supply certainly results more decisive than those of the average spatial resolutions who can not see all the details of the borders of the stretch of water.

Of cartographic data A georeferenced vectorial digital layer of the district of Abidjan and its municipalities and another vectorial layer relative to the limits of the lagoon Ebri were used. This relation allows a general estimation of the volumes filled according to the average depth of the stretch of water according to the following equation: Downloads Download data is not yet available. La localit de Kueinfla prsente un risque lev.

And even on these spaces filled, some local residents practice the market gardening culture Photo 4. Une etude similaire a t realise par Saley ttldtection al.

Revue de g ographie jointe au Bulletin de la Soci t de g ographie de Lyon et de la r gion lyonnaise. About Me miramargondi View my complete profile. Le risque dinondation par dbordement des cours deau rsulte de la combinaison de la vulnrabilit linondation par le dbordement des cours deau et de lala linondation Saley et al. Introduction au traitement de donnes en Hydrologie.

Thse de doctorat,Universit de Cocody, Abidjan, p. The phenomenon of clogging bays is mainly due to the inflow of runoff that drain to the bays, significant amounts of sands and sludge from the conurbation of Abidjan.

Les bilans personnels et professionnels: Nevertheless, seen the scale of the anthropogenic pressure which practices everywhere from the point of view of water lagunaire, it is imperative that we have a synoptic view on the evolution of the bays of the stretch of water of the lagoon Ebri.

However, it has been subjected to strong anthropogenic pressure, in the case of the work of development and the construction of habitats on its borders causing silting and filling the lagoon Bays. This website uses cookies to improve your experience while you navigate through the website. Out of these cookies, the cookies that are categorized as necessary are stored on your browser as they are as essential for the working of basic functionalities of the website.

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