هيدرولوجية الأحواض الشرقية لبحيرة دربندخان

Abstract EN

Surface water is a reflection of the climatic and topographical conditions of the basins in the study area.

It contributes to the prediction of the torrential water quantities of the basin, the extent of its utilization in the various areas of human use, as well as the assessment of the dangers of torrents on human and natural property.

Since there are no hydrological stations to measure surface runoff of rainwater in the study area, the (Snyder) model has been used to estimate the surface runoff size (The 2006 amendments were based on this study H.M.

Raghunath 2006).

The total runoff volume (1053.7/m3/s) was estimated.

The torrents have been studied , maximum flow, Qualitative peak flow, strength and depth of flow, time of rise and gradual reduction of torrents, Hydrograph curve of the study area basins were drowned .