Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/3612
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dc.contributor.authorGarde, R. J.-
dc.contributor.authorKothyari, U. C.-
dc.date.accessioned2019-09-19T10:30:28Z-
dc.date.available2019-09-19T10:30:28Z-
dc.date.issued1988-
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/3612-
dc.description.abstractAnnual flood peak series at 93 stations located all over India have been analysed. Out of the various frequency distributions available, it is found that GEV type I fits the data more closely. It is then found that flood with return period 2.33 yr (Q 2.33) is related to catchment area A, catchment slope S, percent area covered by Forest AF and P, where, P is 2 yr; 45mt, 3 hr, 6 hr or 24 hr rainfall depending on A/S value. It is also found that the coefficient of variation of flood series is related to coefficient of variation of maximum monthly rainfall series in the catchment.en_US
dc.language.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.subjectFlood estimationen_US
dc.subjectRegional flood frequency analysisen_US
dc.titleTheme-3-1-Flood estimation using regional flood frequency analysis.en_US
dc.typeTechnical Reporten_US
Appears in Collections:International Seminar on Hydrology of Extremes (Floods & Low Flows) 1-3 December 1988 at Roorkee (India)

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