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dc.contributor.authorMishra, Siddhartha Shankar-
dc.date.accessioned2014-11-21T10:29:30Z-
dc.date.available2014-11-21T10:29:30Z-
dc.date.issued2010-
dc.identifier.urihttp://hdl.handle.net/123456789/9974-
dc.guideGoel, N. K.-
dc.guideGangopadhyay, Adit-
dc.description.abstractIn a flood hydrograph, the main variables are flood peak, volume, and duration. These three variables of floods are random in nature and are mutually correlated. The joint distributions of these variables are important in hydrologic design. In this study, the joint distribution of flood peak and volume, flood peak and duration, and flood volume and duration have been derived using the copulas. The benefit of using copulas is that it can join different distribution of different flood variables in a common marginal distribution. In this study, the copula method is also used to determine the conditional return periods by using 31 years stream flow data of Naramada River at Garudeshwar, Gujarat, Indiaen_US
dc.subjectHYDROENERGYen_US
dc.subjectBIVARIATE FLOOD FREQUENCY ANALYSISen_US
dc.subjectCOPULASen_US
dc.subjectFLOOD HYDROGRAPHen_US
dc.titleBIVARIATE FLOOD FREQUENCY ANALYSIS USING COPULASen_US
dc.typeM.Tech Dessertationen_US
dc.accession.numberG20104en_US
Appears in Collections:MASTERS' THESES (Hydrology)

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