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- W67682309 abstract "Abstract In modeling of streamflow, there are many difficulties. Such as: rainfalls occurring after from starting of recession, snow melts, interflow, properties of the aquifer recharging the stream, evapotranspiration, geological structure of the and plants on the catchment. However, identification of response of the baseflow affecting stream hydrograph is important for evaluation of water resources. In this study, the procedures, which are used at separation of baseflow, are considered, and a procedure for this purpose is suggested. These procedures are compared each other. Key Words: Baseflow, hydrograph separation, recession, procedure, streamflow, groundwater, Koprucay. Introduction Analyses on the streamflow are carried a great importance due to the increasing of demanding water. The recession work on the streamflow, which are on of these, is especially necessary in determination of low streamflow characteristics. Recession studies are provided limit values on subjects such as water supply, irrigation, hydropower, water quality, etc. For the these reasons, the surface water during the rainy periods may be stored in order to supply of the demanding water during the dry periods. Characteristic of recession curve on the streamflow is shown the difference respect to annuals and even seasons depending rainfalls, snow melts, subsurface water, type and properties of the aquifer, evapotranspiration, geology and plants on the basin. Similarly, characteristic of the recession curve on the baseflow is also shown the difference respect to annuals and even seasons depend in the seepages from rainfall and snowmelt and the discharges which is withdrawn by pumps and galleries. Knowing of the behaviour of baseflow is important in order to control the streamflow recession. While the precise form of a baseflow hydrograph is dependent upon hydrological and geomorphological conditions, the general shape of a baseflow recession continues after the rise of the stream hydrograph may be characterized by: (1) baseflow recession continues after the rise of the stream hydrograph due to the initial outflow from the stream into the adjacent banks; (2) baseflow will peak after the stream hydrograph peak due to the storage – routing effect of the subsurface stores; (3) the baseflow recession will most likely follow an exponential decay function; and (4) the baseflow hydrograph will rejoin the stream hydrograph as direct runoff ceases (Nathan & McMahon, 1990). For time to the peak and periods of the rising limb and recession of the baseflow, various studies were made on forms of baseflow. Studies with this subject are taken into consideration below, and a new procedure is suggested." @default.
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- W67682309 date "2004-01-01" @default.
- W67682309 modified "2023-09-27" @default.
- W67682309 title "A Procedure For Separation Of Baseflow" @default.
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