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dc.contributor.author Bilozor, Walter en_US
dc.date.accessioned 2012-05-14T18:04:05Z
dc.date.available 2012-05-14T18:04:05Z
dc.date.issued 1972 en_US
dc.identifier ocm72750097 en_US
dc.identifier.uri http://hdl.handle.net/1993/5789
dc.description.abstract Although the intense, short duration summer rainstorms falling on the Wilson Creek Watershed in Manitoba, result in a rapid sortm runoff, indicating the possibility of a quick-impulse-response linear relationship, the scatter of points on a simple correlation of rainfall-runoff indicates some large effects of other hydrologic parameters. This study attempts to determine the major parameter affecting this storm rainfall - storm runoff relationship. Three techniques of groundwater separation are considered for derivation of direct storm runoff values. An arbitrary groundwater separation technique with the aid of a composite recession curve is selected in the final analysis. The findings point out that the antecedent basin moisture, as represented by a depth to groundwater table parameter, is the major parameter affecting the storm rainfall - runoff process in the Wilson Creek Watershed. A preliminary attempt to derive a unit hydrograph for the basin indicates that both the peak and its time distribution are variable. en_US
dc.format.extent ix, 97 p. en_US
dc.language en en_US
dc.rights en_US
dc.rights info:eu-repo/semantics/openAccess
dc.title Storm rainfall-runoff relations in Wilson Creek Watershed, Manitoba en_US
dc.type info:eu-repo/semantics/masterThesis
dc.degree.discipline Civil Engineering en_US


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