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@article{ART001747904},
author={Chae，Soo-Kwon and Seungjin Maeng and 황주하 and 김태우 and 김형산},
title={Parameter Estimation of Unit Hydrograph for Derivation of Probable Maximum Flood},
journal={Crisisonomy},
issn={2466-1198},
year={2013},
volume={9},
number={2},
pages={147-162}

TY - JOUR
AU - Chae，Soo-Kwon
AU - Seungjin Maeng
AU - 황주하
AU - 김태우
AU - 김형산
TI - Parameter Estimation of Unit Hydrograph for Derivation of Probable Maximum Flood
JO - Crisisonomy
PY - 2013
VL - 9
IS - 2
PB - Crisis and Emergency Management: Theory and Praxis
SP - 147
EP - 162
SN - 2466-1198
AB - In this study, optimum parameters of Unit Hydrograph for the systematic and reasonable derivation of PMF (probable Maximum Flood) were estimated using the HEC-HMS model as a rainfall-runoff model in Boryeong Dam watershed. As a result, the time of concentration was estimated to be 2.21 hr using the Kraven(Ⅱ) equation and the storage constant was estimated to be 1.92 using the Sabol equation. The CN was estimated to be 80 under AMC-Ⅲ as an antecedent moisture condition. The result of the sensitivity analysis was that the sensitivity of the time of concentration and storage constant was similar each showed a different parameter range. The experiment conditions were divided on time of concentration and storage constant, which affects the PMF regarding the Boryeong Dam watershed. In the HEC-HMS model, the optimum parameter value on the Clark Unit Hydrograph was estimated. The result using Maximum Unit Hydrograph was that the time of concentration was estimated to be 1.68 hr and the storage constant was estimated to be 1.49. Therefore, considering the recent onset of climate change, in designing large scale hydraulic, it is better to use PMF estimated based on the "Maximum Unit Hydrograph" concept under the time of concentration and storage constant condition.
KW - rainfall;runoff;HEC-HMS;probable maximum precipitation;probable maximum flood
DO -
UR -
ER -

Chae，Soo-Kwon, Seungjin Maeng, 황주하, 김태우 and 김형산. (2013). Parameter Estimation of Unit Hydrograph for Derivation of Probable Maximum Flood. Crisisonomy, 9(2), 147-162.

Chae，Soo-Kwon, Seungjin Maeng, 황주하, 김태우 and 김형산. 2013, "Parameter Estimation of Unit Hydrograph for Derivation of Probable Maximum Flood", Crisisonomy, vol.9, no.2 pp.147-162.

Chae，Soo-Kwon, Seungjin Maeng, 황주하, 김태우, 김형산 "Parameter Estimation of Unit Hydrograph for Derivation of Probable Maximum Flood" Crisisonomy 9.2 pp.147-162 (2013) : 147.

Chae，Soo-Kwon, Seungjin Maeng, 황주하, 김태우, 김형산. Parameter Estimation of Unit Hydrograph for Derivation of Probable Maximum Flood. 2013; 9(2), 147-162.

Chae，Soo-Kwon, Seungjin Maeng, 황주하, 김태우 and 김형산. "Parameter Estimation of Unit Hydrograph for Derivation of Probable Maximum Flood" Crisisonomy 9, no.2 (2013) : 147-162.

Chae，Soo-Kwon; Seungjin Maeng; 황주하; 김태우; 김형산. Parameter Estimation of Unit Hydrograph for Derivation of Probable Maximum Flood. Crisisonomy, 9(2), 147-162.

Chae，Soo-Kwon; Seungjin Maeng; 황주하; 김태우; 김형산. Parameter Estimation of Unit Hydrograph for Derivation of Probable Maximum Flood. Crisisonomy. 2013; 9(2) 147-162.

Chae，Soo-Kwon, Seungjin Maeng, 황주하, 김태우, 김형산. Parameter Estimation of Unit Hydrograph for Derivation of Probable Maximum Flood. 2013; 9(2), 147-162.

Chae，Soo-Kwon, Seungjin Maeng, 황주하, 김태우 and 김형산. "Parameter Estimation of Unit Hydrograph for Derivation of Probable Maximum Flood" Crisisonomy 9, no.2 (2013) : 147-162.