Confidence intervals for expected moments algorithm flood quantile estimates
By T. Cohn, W. L. Lane, Jery R. Stedinger. 2001
93 citations recorded by the source corpus.
Subfields: Ecology, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/5280632fe5f42b50b321b051878f6946f83874d5
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Ecology
- Dirceu Silveira Reis
- Jery R. Stedinger
- J. England
- J. Salas
- Zhongmin Liang
- R. D. Jarrett
- Binquan Li
- Veronica W. Griffis
In Global and Planetary Change
- Jery R. Stedinger
- Dirceu Silveira Reis
- Veronica W. Griffis
- Zhongmin Liang
- Binquan Li
- Wenjuan Chang
- J. Salas
- J. England
Citations in the corpus
- Log Pearson type 3 quantile estimators with regional skew information and low outlier adjustments (2004, methodology): “EMA flood quantile estimators were developed by Cohn et al. [2001] .”
- Bayesian flood frequency analysis in the light of model and parameter uncertainties (2012, methodology): “In the methods, uncertainties are mainly characterized by the approximate confidence intervals (Stedinger 1983; Chowdhury and Stedinger 1991; Stedinger et al. 1993; Ashkar and Ouarda 1998; Whitley and Hromadka 1999; Cohn et al. 2001).”
- Bayesian MCMC flood frequency analysis with historical information (2005, methodology): “A drawback of the MLE approach is that it does not always work well, such as when fitting a Log-Pearson Type 3 distribution (Cohn et al., 2001).”
- Comparisons of two moments‐based estimators that utilize historical and paleoflood data for the log Pearson type III distribution (2003, methodology): “The ERL is defined as [Cohn et al., 1997] ERLT s; hð Þ ¼ s MSE X̂T s; h ¼ 0h i MSE X̂T s; h;Xoh i ð18Þ The ERL is defined as the number of years of systematic data that would produce the same MSE as the given combination of historical and systematic data combined [Cohn, 1984].”