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dc.contributor.authorDripchak, Mark Meyers,1958-*
dc.creatorDripchak, Mark Meyers,1958-en_US
dc.date.accessioned2011-11-28T14:16:08Z
dc.date.available2011-11-28T14:16:08Z
dc.date.issued1992en_US
dc.identifier.urihttp://hdl.handle.net/10150/192069
dc.description.abstractThe effects of rainfall intensity distribution on runoff hydrographs were studied for 89 watersheds, using event data obtained from the USDA-ARS. Treating the hyetograph and hydrograph as frequency distributions, their shapes were described by the first four statistical moments. A number of other measures of the rainfall and runoff were calculated (rainfall depth and duration, maximum 15-minute intensity, watershed moisture status; runoff depth and duration, peak runoff rate, peak rate relative to event rainfall and runoff depths, runoff ratio, and runoff Curve Number). The rainfall moments and measures were compared to those of the hydrographs, and statistical associations were drawn. The first two moments of the hyetograph and hydrograph were significantly correlated, while the shape parameters of skew and peakedness were less so. The dispersion of the rainfall intensity distribution is a significant factor affecting the correlations between the commonly studied parameters mentioned above.
dc.language.isoenen_US
dc.publisherThe University of Arizona.en_US
dc.rightsCopyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author.en_US
dc.subject.lcshHydrology.en_US
dc.subject.lcshRainstorms.en_US
dc.subject.lcshHydrography.en_US
dc.titleAssociative relationships between moments of rainstorms and the corresponding hydrographs.en_US
dc.typeThesis-Reproduction (electronic)en_US
dc.typetexten_US
dc.identifier.oclc221707216en_US
thesis.degree.grantorUniversity of Arizonaen_US
thesis.degree.levelmastersen_US
dc.contributor.committeememberHawkins, Richard H.en_US
dc.contributor.committeememberRenard, Kenneth G.en_US
dc.contributor.committeememberLopes, Vicente L.en_US
thesis.degree.disciplineRenewable Natural Resourcesen_US
thesis.degree.disciplineGraduate Collegeen_US
thesis.degree.nameM.S.en_US
dc.description.notehydrology collectionen_US
refterms.dateFOA2018-06-29T07:40:43Z
html.description.abstractThe effects of rainfall intensity distribution on runoff hydrographs were studied for 89 watersheds, using event data obtained from the USDA-ARS. Treating the hyetograph and hydrograph as frequency distributions, their shapes were described by the first four statistical moments. A number of other measures of the rainfall and runoff were calculated (rainfall depth and duration, maximum 15-minute intensity, watershed moisture status; runoff depth and duration, peak runoff rate, peak rate relative to event rainfall and runoff depths, runoff ratio, and runoff Curve Number). The rainfall moments and measures were compared to those of the hydrographs, and statistical associations were drawn. The first two moments of the hyetograph and hydrograph were significantly correlated, while the shape parameters of skew and peakedness were less so. The dispersion of the rainfall intensity distribution is a significant factor affecting the correlations between the commonly studied parameters mentioned above.


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