GENETIC DETERMINATION OF THE MAIN COMPONENTS OF THE MEAN INTERANNUAL FLOW WADIS IN THE SEMI-ARID CLIMATE OF THE MAGHREB

dc.contributor.authorM., Ladjel
dc.date.accessioned2023-05-29T10:21:36Z
dc.date.available2023-05-29T10:21:36Z
dc.date.issued2020-05-01
dc.descriptionarticalen_US
dc.description.abstractNorth of the Maghreb, the flow of the wadis is generated by the rains. The hydro-climatic network is not dense enough to reasonably estimate the flow in any watershed where the wadis are not gauged. There is a need to develop methods for the acceptable estimation of river flow. The average flow of wadis is conditioned by a combination of climatic factors and local physicogeographic and hydrogeological factors. The influence of these local factors is dominant on the small and medium watersheds through the subterranean supply, where the climatic factors determine the superficial flow. The mean interannual flow (MIF) is composed of a regional climatic flow and a potential local flow. Regional climate flow differs from the actual climate flow in a watershed. The objective of this research is the genetic determination of the main components of the average interannual flow of wadis in the semi-arid climate of the Maghreb.en_US
dc.identifier.citationM. Ladjel. GENETIC DETERMINATION OF THE MAIN COMPONENTS OF THE MEAN INTERANNUAL FLOW WADIS IN THE SEMI-ARID CLIMATE OF THE MAGHREB. Journal of Fundamental and sciences. vol.10, no 2. May 2018. Faculty of exact sciences. university of el oued. [visited in 01/05/2018. available from [copy the link here]en_US
dc.identifier.urihttp://dspace.univ-eloued.dz/handle/123456789/24758
dc.language.isoenen_US
dc.publisheruniversity of eloued جامعة الواديen_US
dc.relation.ispartofseries1112-9867;
dc.subjectflow, rain, climate, evapotranspiration, infiltration.en_US
dc.titleGENETIC DETERMINATION OF THE MAIN COMPONENTS OF THE MEAN INTERANNUAL FLOW WADIS IN THE SEMI-ARID CLIMATE OF THE MAGHREBen_US
dc.typeArticleen_US

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