1987
DOI: 10.1016/0022-1694(87)90070-9
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A review of methods of parameter estimation for the extreme value type-1 distribution

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Cited by 58 publications
(22 citation statements)
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“…The variance of the T-year event estimator due to sampling uncertainty in this case is given by Phien (1987) as Varfx x T g ¼ a 2 n À 1 1:11 À 0:907 n þ 0:457 À 1:17 n y T þ 0:805 À 0:186 n y 2 T ! ð9Þ…”
Section: Methods Of Probability Weighted Momentsmentioning
confidence: 99%
See 1 more Smart Citation
“…The variance of the T-year event estimator due to sampling uncertainty in this case is given by Phien (1987) as Varfx x T g ¼ a 2 n À 1 1:11 À 0:907 n þ 0:457 À 1:17 n y T þ 0:805 À 0:186 n y 2 T ! ð9Þ…”
Section: Methods Of Probability Weighted Momentsmentioning
confidence: 99%
“…The extreme value type I (EV-I) distribution is commonly used for estimation of extreme hydrological events, see for example Jain and Singh (1987) and Phien (1987). At-site estimation of extreme events is often hampered by lack of information leading to increased prediction uncertainty in the estimation of Tyear events.…”
Section: Introductionmentioning
confidence: 99%
“…But, the method has the disadvantage of frequently giving biased estimates and often failed to give the desired accuracy in estimating extremes from hydrological data. It may not produce good estimators in small samples, especially when the random variable is restricted to an interval that depends on the parameters [4][5][6]. PWM and MLS are much less complicated, and the computations are simpler.…”
Section: Introductionmentioning
confidence: 99%
“…The regional models developed could be successfully used in predicting flood quantiles needed in hydrological design for ungauged catchments within the region studied and without any available historic flood information. The assumption that the missing annual flood flows at the sites of interest fit the EV1 distribution is considered to be a reasonable approximation justified by the hydrological experience from the region and by the wide applicability of the EV1 distribution in analysing annual extremes (Phien, 1987). The models, as for all regional models, cannot take into account future changes in the catchments and cannot be safely applied outside the region of the study.…”
Section: Prediction Of Flood Quantiles For Ungauged Catchmentsmentioning
confidence: 99%