Maximum Runoff Of The Flood On Wadis Of Northern Part Of Algeria

dc.contributor.authorLadjel, M.
dc.contributor.authorGopchenko, E. D.
dc.contributor.authorOvcharuk, V. A.
dc.date.accessioned2020-10-21T08:40:19Z
dc.date.available2020-10-21T08:40:19Z
dc.date.issued2014-01-01
dc.descriptionArticale in Journal of fundamental and Applied Sciences Vol. 06 N. 01en_US
dc.description.abstractWadis of Algeria are characterized by a very irregular hydrological regime. The question of estimating the maximum flow of wadis is relevant. We propose in this paper a method based on an interpretation of the transformation of surface runoff in streamflow. The technique of account the maximal runoff of flood for the rivers of northern part of Algeria based on the theory of channel isochrones is offered.The realization of this method is performed on the basis of hydrometeorological data standarts.en_US
dc.identifier.citationArticale in Journal of fundamental and Applied Sciences Vol. 06 N. 01en_US
dc.identifier.issn1112-9867
dc.identifier.urihttps://dspace.univ-eloued.dz/handle/123456789/7208
dc.language.isoenen_US
dc.publisherUniversity of Eloued جامعة الواديen_US
dc.subjectwadis, maximum flow, runoff, streamflow, flood.en_US
dc.titleMaximum Runoff Of The Flood On Wadis Of Northern Part Of Algeriaen_US
dc.typeArticleen_US

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