Preprints
https://doi.org/10.5194/hess-2018-380
https://doi.org/10.5194/hess-2018-380
12 Dec 2018
 | 12 Dec 2018
Status: this preprint has been withdrawn by the authors.

Copula and ARMA based study of controlled outflow at Farakka barrage

Uttam Singh, Venkappayya R. Desai, Pramod K. Sharma, and Chandra S. P. Ojha

Abstract. In this study, 25 years mean monthly out flow discharge data of Farakka barrage was used (i.e., from 1949 to 1968). Farakka barrage is located between on Ganga River. Spatial and temporal variation in flow rate for any particular area is very common due to various meteorological and other factors existing in nature. But large variations in these factors cause extreme events (e. g., floods and droughts). Monthly outflow discharge for a particular critical month are predicted using statistical models (ARMA Model and Copula Model). Different Copulas (i.e., Normal, t, Frank, Clayton, Gumbel–Hoggard, Ali–Mikhail–Haq) are used for this purpose and the copula model is selected based on distribution functions (Normal distribution, Lognormal distribution, Extreme value type-1 distribution, Generalized Extreme value type, Gamma distribution, Weibull distribution, Exponential distribution). The distribution is selected based on the Mean square error (MSE), Akaike Information Criterion (AIC), and Bayesian Information Criterion (BIC). The model parameters were computed using the Maximum Likelihood (ML) estimation method.

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Uttam Singh, Venkappayya R. Desai, Pramod K. Sharma, and Chandra S. P. Ojha

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
Uttam Singh, Venkappayya R. Desai, Pramod K. Sharma, and Chandra S. P. Ojha
Uttam Singh, Venkappayya R. Desai, Pramod K. Sharma, and Chandra S. P. Ojha

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Short summary
In this study, 25 years mean monthly out flow discharge data of Farakka barrage was used (i.e., from 1949 to 1968). Farakka barrage is located between on Ganga River. Spatial and temporal variation in flow rate for any particular area is very common due to various meteorological and other factors existing in nature.