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- W4214936580 abstract "Streamflow that is usually measured at a stream gauging station is made up of baseflow, which is sourced from groundwater aquifers, snowmelt, previous storm, and quickflow or direct flow, which comes from surface runoff due to excess rainfall. A hydrograph is a continuous plot of the instantaneous discharge against time. It results from a combination of the physiographic and meteorological conditions in a watershed and represents the integrated effects of climate, hydrologic losses, surface runoff, interflow, and groundwater flow. Detailed analysis of hydrographs is usually important in flood damage mitigation, flood forecasting, or establishing the design flows for structures that convey floodwaters. Streamflow that is usually observed on the river is composed of quickflow and baseflow. Baseflow separation research is regarded as one of the most important and difficult issues in hydrology and ecohydrology but lacked unified standards in the concepts and methods. The objectives of this chapter are to explain the flood hydrograph and the factors affecting its form. Its highlights are the graphical, digital filters, and tracer-based methods used to separate the baseflow from quickflow. Finally, it demonstrates how baseflow can be separated from quickflow using the web-based hydrological hydrograph analysis tool (WHAT) using daily data from the Mutirikwi River in Zimbabwe." @default.
- W4214936580 created "2022-03-05" @default.
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- W4214936580 date "2022-03-04" @default.
- W4214936580 modified "2023-09-23" @default.
- W4214936580 title "Flood Hydrograph and Baseflow Separation Using the Web- Based Hydrograph Analysis Tool" @default.
- W4214936580 doi "https://doi.org/10.1201/9781003262640-24" @default.
- W4214936580 hasPublicationYear "2022" @default.
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