Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/3456
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dc.contributor.authorSingh, R. D.-
dc.contributor.authorMishra, S. K.-
dc.date.accessioned2019-08-30T10:56:10Z-
dc.date.available2019-08-30T10:56:10Z-
dc.date.issued1991-
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/3456-
dc.description.abstractFor the estimation of design flood for any water resources project, the hydrologist often needs to have a fairly reliable es1 1 a of design storm. Among the various methods used for the estimation of design storm the commonly used methods are : (i ) Depth-duration (DD) analysis (ii ) Depth-area'duration (DAD) analysis (iii ) Storm transposition The depths obtained by any one of these methods are maximised for moisture content to obtain the probable maximum precipitation (PMP) estir ,s. Subsequently the PMP values are distributed into shorter t intervals and arranged in order to get design sequence the storm at shorter time intervals. This lecture describeS the physical methods of estimation of design storm alongwith moisture maximisation for estimating the probable maximum precipitation (PMP). Further the technique of distribution of the PMP into shorter intervals would also described.en_US
dc.language.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.subjectFlood studiesen_US
dc.subjectDepth duration analysisen_US
dc.subjectTime distributionen_US
dc.subjectEnvelope curvesen_US
dc.title5-Chapter-V-Design flood studiesen_US
dc.typeTechnical Reporten_US
Appears in Collections:Regional course on Project Hydrology : Course material

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