• Title/Summary/Keyword: hydraulic flood routing

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Flood Hazard Map in Woo Ee Stream Basin Using Conclusive Hydraulic Routing Model (결정론적 홍수위 추적 모형을 이용한 우이천 유역의 홍수범람도 작성)

  • Moon, Young-Il;Yoon, Sun-Kwon;Kim, Jae-Hyun;Ahn, Jae-Hyun
    • 한국방재학회:학술대회논문집
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    • 2008.02a
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    • pp.637-640
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    • 2008
  • Flood control and river improvement works are carried out every year for the defense of the flood disaster, it is impossible to avoid the damage when there is a flood exceeding the capacity of hydraulic structures. Therefore, nonstructural counter plans such as the establishment of flood hazard maps, the flood warning systems are essential with structural counter plans. In this study, analysis of the internal inundation effect using rainfall runoff model such as PC-SWMM was applied to Woo Ee experimental stream basin. Also, the design frequency analysis for effects of the external inundation was accomplished by main parameter estimation for conclusive hydraulic routing using HEC-RAS model. Finally, inundated areas for flood hazard map were estimated at Woo Ee downstream basin according to flood frequency using HEC-GeoRAS model linked by Arc View GIS.

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DEVELOPMENT OF A REAL-TIME FLOOD FORECASTING SYSTEM BY HYDRAULIC FLOOD ROUTING

  • Lee, Joo-Heon;Lee, Do-Hun;Jeong, Sang-Man;Lee, Eun-Tae
    • Water Engineering Research
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    • v.2 no.2
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    • pp.113-121
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    • 2001
  • The objective of this study is to develop a prediction mode for a flood forecasting system in the downstream of the Nakdong river basin. Ranging from the gauging station at Jindong to the Nakdong estuary barrage, the hydraulic flood routing model(DWOPER) based on the Saint Venant equation was calibrated by comparing the calculated river stage with the observed river stages using four different flood events recorded. The upstream boundary condition was specified by the measured river stage data at Jindong station and the downstream boundary condition was given according to the tide level data observed at he Nakdong estuary barrage. The lateral inflow from tributaries were estimated by the rainfall-runoff model. In the calibration process, the optimum roughness coefficients for proper functions of channel reach and discharge were determined by minimizing the sum of the differences between the observed and the computed stage. In addition, the forecasting lead time on the basis of each gauging station was determined by a numerical simulation technique. Also, we suggested a model structure for a real-time flood forecasting system and tested it on the basis of past flood events. The testing results of the developed system showed close agreement between the forecasted and observed stages. Therefore, it is expected that the flood forecasting system we developed can improve the accuracy of flood forecasting on the Nakdong river.

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Flood Analysis in the Tidal Reaches of the Nakdong River (낙동강 하류부의 감조구간에 대한 홍수해석)

  • Lee, Joo-Heon;Lee, Eun-Tae;Lee, Do-Hun;Kim, Nam Won
    • Journal of Korea Water Resources Association
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    • v.31 no.3
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    • pp.235-242
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    • 1998
  • The objective of this study is to develope a predictive model for flood forecasting in the tidal reaches of the Nakdong river and to analyze the tidal effects of major flood forecasting station of the Nakdong river by using the hydraulic flood routing. In the calibration process the optimum roughness coefficients as functions of channel reach and discharge were determined and the calibration results suggest that the unsteady hydraulic flood routing model simulated with the optimum roughness coefficients showed close agreement between the calculated and observed stage.

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A Forecasting Model for the Flood Peak Stage and Flood Travel Time by Hydraulic Flood Routing

  • Yoon, Yong-Nam;Park, Moo-Jong
    • Korean Journal of Hydrosciences
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    • v.4
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    • pp.11-19
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    • 1993
  • The peak flood discharge at a downstream station and the flood travel time between a pair of dams due to a specific flood release from the upper reservoir are computed using a hydraulic river channel routing method. The study covered the whole large reservoir system in the Han River, Korea. The computed flood discharges and the travel times between dams were correlated with the duration and the magnitude of flood release rate at the upstream reservoir, and hence a multiple regression model is proposed for each river reach between a pair of dams. The peak flood discharge at a downstream location can be converted to the peak flood stage by a rating curve. Hence, the proposed regression model could be used to forecast the peak flood stage at a downstream location and the flood travel time between dams using the information on the flood travel time, release rate and duration from the upper dam.

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Flood Forecasting Study using Neural Network Theory and Hydraulic Routing (신경망 이론과 수리학적 홍수추적에 의한 홍수예측에 관한 연구)

  • Jee, Hong Kee;Choo, Yeon Moon
    • Journal of Korea Water Resources Association
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    • v.47 no.2
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    • pp.207-221
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    • 2014
  • Recently, due to global warming, climate change has affected short time concentrated local rain and unexpected heavy rain which is increasingly causing life and property damage. Therefore, this paper studies the characteristic of localized heavy rain and flash flood in Nakdong basin study area by applying Data Mining method to predict flood and constructing water level predicting model. For the verification neural network from Data Mining method and hydraulic flood routing was used for flood from July 1989 to September 1999 in Nakdong point and Iseon point was used to compare flood level change between observed water level and SAM (Slope Area Method). In this research, the study area was divided into three cases in which each point's flood discharge, water level was considered to construct the model for hydraulic flood routing and neural network based on artificial intelligence which can be made from simple input data used for comparison analysis and comparison evaluation according to actual water level and from the model.

Forecasting of Peak Flood Stage at Downstream Location and the Flood Travel Time by Hydraulic Flood Routing (수리학적 홍수추적에 의한 댐 방류시 하류수위 및 주요 하도구간별 홍수도달 시간의 예측)

  • 윤용남;박무종
    • Water for future
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    • v.25 no.3
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    • pp.115-124
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    • 1992
  • The peak flood discharge at a downstream station and the flood travel time between a pair of dams due to a specific flood release from the upper reservoir are computed using a hydraulic river channel routing method. The study covered the whole reservoir system in the Han River. The computed peak flood discharges and the travel times between dams were correlated with the duration and the magnitude of flood release rate at the upstream reservoir, and hence a multiple regression model is proposed for each river reach between a pair of dams. The peak flood discharge at a downstream location can be converted to the peak flood stage by rating curve. Hence, the proposed regression model could be used to forecast the peak flood stage at a downstream location and the flood travel time between dams using the information on the flood release rate and duration from the upper dam.

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A Study on Channel Flood Routing Using Nonlinear Regression Equation for the Travel Time (비선형 유하시간 곡선식을 이용한 하도 홍수추적에 관한 연구)

  • Kim, Sang Ho;Lee, Chang Hee
    • Journal of Wetlands Research
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    • v.18 no.2
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    • pp.148-153
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    • 2016
  • Hydraulic and hydrological flood routing methods are commonly used to analyze temporal and spatial flood influences of flood wave through a river reach. Hydrological flood routing method has relatively more simple and reasonable performance accuracy compared to the hydraulic method. Storage constant used in Muskingum method widely applied in hydrological flood routing is very similar to the travel time. Focusing on this point, in this study, we estimate the travel time from HEC-RAS results to estimate storage constant, and develop a non-linear regression equation for the travel time using reach length, channel slope, and discharge. The estimated flow by Muskingum model with storage constant of nonlinear equation is compared with the flow calculated by applying the HEC-RAS 1-D unsteady flow simulation. In addition, this study examines the effect on the weighting factor changes and interval reach divisions; peak discharge increases with the bigger weighting factor, and RMSE decreases with the fragmented division.

The Establishment and Application of Hydraulic Channel Routing Model on the Nakdong River (I) Theory and Evaluation of Travel Time (낙동강 유역 수리학적 하도추적 모형 구축 및 적용 (I) 이론 및 도달시간 산정)

  • Lee, Eul Rae;Shin, Chul Kyun;Kim, Sang Ho
    • Journal of Wetlands Research
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    • v.8 no.1
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    • pp.73-82
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    • 2006
  • In this study, the hydraulic channel routing model is applied to analyze water surface elevation pattern on the Nakdong river in flood cases. The procedure to apply FLDWAV model is presented to solve the Saint-Venant Equations by using four points implicit finite differential scheme. And the flood travel time is studied for reasonable dam management. As this results, variable assumption and constraint are followed to evaluate flood travelling time by hydraulic model. A guideline of reasonable dam's decision making considering downstream effect is showed by this constructed model, and scientific hydraulic analysis is possible by it.

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A Study on the Flood Routing using a Convective-Diffusion Model (대류-확산 모델을 이용한 홍수추적에 관한 연구)

  • 남선우;박상우
    • Water for future
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    • v.18 no.3
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    • pp.265-270
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    • 1985
  • The prediction of a design-flood hydrograph at a particular site on a river may be based on the derivation of discharge or stage hydrograph at an upstream section, togeater with a method to route this hydrograph along the rest of river. On the other hand, flood routing methods provide a useful tool for the analysis of flooding in all but the smaller catchment, and these methods are largely stored into hydrological method and hydraulic method. Although the Muskingum Method as a hydrological method ignores dynamic effects on the flood wave, Muskingum-Cunge Method based on hydraulic method is possible to improve the method so that it gives a good approximation to the solution of the linear convective-diffusion equation. This is made on the basis of the finite diffeience equation for the Muskingum Method. In the study, the outflows predicted by Muskingum-Cunge Method are campared with the observed outflows of the Pyung Chang River.

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An Analysis of Hydraulic Characteristics of Drainage Sub-Canal at Large-Sized Paddy Fields (대구획 경지정리지구의 배수지거 수리특성)

  • Kang, Min-Goo;Park, Seung-Woo
    • Proceedings of the Korean Society of Agricultural Engineers Conference
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    • 2001.10a
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    • pp.74-79
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    • 2001
  • A one-dimensional flood routing model was formulated to simulate the flood flow of drainage sub-canal using the continuity equation of paddy field and the momentum and continuity equation of drainage sub-canal. The model was applied for evaluating the hydraulic characteristics of drainage sub-canal at large-sized paddy fields. The model applicability was evaluated with field data and the simulated results were in good agreement with the observed data.

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