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SHORT TERM VARIATION OF RUNOFF-RAINFALL RATIOS IN NOVA SCOTIA IHD WATERSHEDS

dc.contributor.authorTürker, Yücel
dc.contributor.copyright-releaseYesen_US
dc.contributor.degreeMaster of Scienceen_US
dc.contributor.departmentDepartment of Earth and Environmental Sciencesen_US
dc.contributor.ethics-approvalNot Applicableen_US
dc.contributor.external-examinern/aen_US
dc.contributor.graduate-coordinatorn/aen_US
dc.contributor.manuscriptsNot Applicableen_US
dc.contributor.thesis-readern/aen_US
dc.contributor.thesis-supervisorn/aen_US
dc.date.accessioned2023-02-23T20:44:25Z
dc.date.available1969
dc.date.defence1969
dc.date.issued1969
dc.description.abstractRunoff-rainfall ratios are estimated from streamflow hydrographs using precipitation and streamflow data for three IHD watersheds in Nova Scotia. The study watersheds are located in eastern, central and western Nova Scotia. Instrumentation for the measurement of precipitation, temperature and streamflow was installed in the watersheds as part of the International Hydro logical Decade program. Annual hydrographs were plotted and separated into their direct runoff and groundwater runoff components. Average annual direct runoff varied from 20 to 29.8 inches and groundwater runoff varied from 11.3 to 28.7 inches. Individual and largest storms were selected for each month from the meteorological records (Fraser Brook 3 years, April Brook 2 years, Sharpe Brook 1 year of period). Storm hydrographs were also plotted and separated into their two components of direct and groundwater runoff. Ratios of direct runoff to average weighted rainfall were determined for each watershed. Estimates revealed that these ratios varied from 0. 03 to 29% for the period of study. Annual runoff-rainfall ratio in the watersheds varied from 66 to 97%.en_US
dc.identifier.urihttp://hdl.handle.net/10222/82304
dc.titleSHORT TERM VARIATION OF RUNOFF-RAINFALL RATIOS IN NOVA SCOTIA IHD WATERSHEDSen_US

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