Please use this identifier to cite or link to this item: http://localhost:8081/jspui/handle/123456789/11553
Full metadata record
DC FieldValueLanguage
dc.contributor.authorGoswami, Ajoy-
dc.date.accessioned2014-11-27T05:15:38Z-
dc.date.available2014-11-27T05:15:38Z-
dc.date.issued1979-
dc.identifierM.Techen_US
dc.identifier.urihttp://hdl.handle.net/123456789/11553-
dc.guideSeth, S. M.-
dc.description.abstractThe process of conversion of rainfall excess into direct runoff has been studied using two modelling approaches. The translation effect and areal non-uniformity of rainfall has been consided by dividing the catchment into subareas by means of isochrones. In the first approach, the storage effect has been simulated by translation coefficients which subdivide the excess rainfall generated over a subarea dur-ing a particular time interval. In the second approach, hydrologic routing of Muskingum type has been used to simulate the storage effect. The performance of model in simulating observed runoff for a small catchment is better in case of second approach.en_US
dc.language.isoenen_US
dc.subjectHYDROLOGYen_US
dc.subjectRAINFALL RUNOFF PROCESSen_US
dc.subjectSMALL CATCHMENTen_US
dc.subjectHYDROLOGIC ROUTINGen_US
dc.titleMODELLING OF RAINFALL RUNOFF PROCESS OF A SMALL CATCHMENTen_US
dc.typeM.Tech Dessertationen_US
dc.accession.number176081en_US
Appears in Collections:MASTERS' THESES (Hydrology)

Files in This Item:
File Description SizeFormat 
HYD176081.pdf5.16 MBAdobe PDFView/Open


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.