Abstract
The Geomorphologic Instantaneous Unit Hydrograph watershed modeling approach is extended to account for subsurface runoff. Watershed response to rainfall is modelled as a Markov process whose parameters can be related to physical watershed characteristics. Time-varying instantaneous unit hydrographs are subsequently derived and convoluted with antecedent rainfall intensities to generate total streamflow discharges. This watershed model was applied to simulate the Little River Watershed in southeast Georgia. Predicted streamflows were found to be in good agreement with streamgage measurements.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
