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Peak basin stream flow resulted from delivery of sub-basins runoff to a spatially linked drainage network during spring snowmelt.
Despite having periods of increased HOF generation, the total HOF contribution from agricultural fields to the basin stream hydrograph is similar in magnitude to that of unpaved roads, which occupy 95% less land area.
In the southwest and in the northern boundary zone of the Puli basin, stream terraces are found.
Survey of India (SOI) toposheet (scale 1 50,000) number 64F/2, 64F/5 and 64F/6 were processed for basin stream and boundary delineation.
The boundary of the basin, stream network and elevation contours of the Dulung-Nala basin up to Phekoghat were mapped using Survey of India toposheets with scales of (1 50,000) and (1 250,000) using ArcGIS module of SMS 6.0 Surface Water Modeling System.
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In the north-central Oregon plateau, known as the Deschutes-Umatilla Plateau, a portion of the Columbia River basin, streams are entrenched and provide some bold relief.
Peak streamflow in the lower basin was most sensitive to the hydraulic conductivity of the confining unit in the upper basin, and the Manning's coefficient of upper basin streams, indicating that all peak storm flows originate in the upper basin.
Both the data was used to update basin streams and watershed boundary.
Linear aspect in morphometry is characterized by basin length, stream order, stream number, stream length and bifurcation ratio.
Hack (1957) identified that for a large number of basins, the stream length and basin area is associated by a simple power function as follows: Lar = 1.4* × A0.6.
It is apparent that pasturelands in this basin affect stream nutrient concentrations and export to Beaver Lake and its tributaries.
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