A NEW APPROCH TO EVALUATING THE EFFECT OF WATERSHED STORAGE ON FLOOD SKEW

dc.contributor.advisorMcCuen, Richard Hen_US
dc.contributor.authorHabete, Danielen_US
dc.contributor.departmentCivil Engineeringen_US
dc.contributor.publisherDigital Repository at the University of Marylanden_US
dc.contributor.publisherUniversity of Maryland (College Park, Md.)en_US
dc.date.accessioned2010-10-07T06:14:59Z
dc.date.available2010-10-07T06:14:59Z
dc.date.issued2010en_US
dc.description.abstractEstimates of flood skew are inaccurate and the inaccuracy influences flood discharge estimates using the log Pearson Type III distribution. The skew map is commonly used despite the fact that it's inaccurate, lacks a conceptual basis, and does not reflect watershed processes. Attempts at regionalizing station skew using regression analysis have only provided marginal improvements in accuracy, possibly because the predictor variables are not good indicators of the physical characteristics that influence the variation in skewness. Therefore, a new approach is needed to improve skew estimates. This research explored the potential of using a distributed model that includes predictor variables that better represent watershed storage. The results showed that watershed storage is the main factor that affects flood skew, and that increases in watershed storage causes flood skews to be algebraically more negative.en_US
dc.identifier.urihttp://hdl.handle.net/1903/10967
dc.subject.pqcontrolledEngineering, Civilen_US
dc.titleA NEW APPROCH TO EVALUATING THE EFFECT OF WATERSHED STORAGE ON FLOOD SKEWen_US
dc.typeThesisen_US

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