• Proceedings of the Korea Water Resources Association Conference
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• 2011.05a
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• pp.380-380
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• 2011

본 연구는 경인 아라뱃길의 운영을 위한 기초자료로써 굴포천 유역에서 분포형 강우 모형을 적용하기 위한 것으로 HEC-HMS의 ModClark 방법을 사용하였다. HEC-HMS에서 사용가능한 강우유출모형 중 ModClark 방법은 격자기반의 공간적 강우 분포 모형으로 본 연구에서는 그 기초 지형격자 자료를 10m DEM을 이용해 ArcGIS에서의 작업을 통해 추출하였다. HEC-HMS에 입력 가능한 격자기반 지형자료를 얻기 위해서 미 공병단에서 배포하는 GIS tool 인 HEC-GeoHMS를 이용하였다. 또한 강우자료는 한국수자원공사의 3km*3km 격자기반의 K-PPM 자료를 사용하였다.

• Journal of The Korean Society of Agricultural Engineers
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• v.50 no.3
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• pp.17-27
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• 2008

In this study, three different unit hydrograph methods (Snyder, SCS, Clark) in the HEC-HMS were compared to find better fit with the observed data in the small agricultural watershed. Baran watershed, having $3.85km^2$ in size, was selected as a study watershed. The watershed input data for HEC-HMS were retrieved using HEC-GeoHMS which was developed to assist making GIS input data for HEC-HMS. Rainfall and water flow data were monitored since 1996 for the study watershed. Fifty five storms from 1996 to 2003 were selected for model calibration and verification. Three unit hydrograph methods were compared with the observed data in terms of simulated peak runoff, peak time and total direct runoff for the selected storms. The results showed that the coefficient of determination ($R^2$) for the observed peak runoff was $0.8666{\sim}0.8736$ and root mean square error, RMSE, was $5.25{\sim}6.37\;m^3/s$ for calibration stages. In the model verification, $R^2$ for the observed peak runoff was $0.8588{\sim}0.8638$ and RMSE was $9.57{\sim}11.80\;m^3/s$, which were slightly less accurate than the calibrated data. The simulated flood hydrographs were well agreed with the observed data. SCS unit hydrograph method showed best fit, but there was no significant difference among the three unit hydrograph methods.

• Proceedings of the Korea Water Resources Association Conference
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• 2005.05b
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• pp.1209-1213
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• 2005

It reflects well feature of slope that is characteristic of city river basin of Pusan local. Process various hydrological datas and basin details datas which is collected through basin basis data. weather satellite equipment(EMS-DEU) and automatic water level equipment(AWS-DEU) and use as basin input data of ILLUDAS model, SWMM model and HEC-HMS model In order to examine outflow feature of experiment basin and then use in reservoir design of experiment basin through calibration and verification about HEC-HMS model. Inserted design rainfall for 30 years that is design criteria of creek into HEC-HMS model and then calculated design floods according to change aspect of the impermeable rate. Capacity of reservoir was determined on the outflow mass curve. Designed imagination reservoir(volume $54,000m^3$) at last outlet upper stream of experiment basin, after designing reservoir. It could be confirmed that the peak flow was reduced resulting from examining outflow aspect. Designing reservoir must decrease outflow of urban areas.

• Proceedings of the Korean Society of Agricultural Engineers Conference
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• 2003.10a
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• pp.483-486
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• 2003

This paper presents how effective the detention storage is to control floods at a test watershed. HEC-HMS model was applied to simulate the effects of the storages of different levels and installation methods on the flood peak reduction. The results showed that the detention storage may significant reduce the flood peaks, and the effectiveness depends on the sizes of the storage and types of installation. The simulated peak values reduce considerably for the design storm events. The results also showed that alternatives to control flood may be evaluated using the model.

• Proceedings of the Korea Water Resources Association Conference
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• 2007.05a
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• pp.1454-1458
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• 2007

The determination of feasible design flood is the most important to control flood damage in river management. Model parameters should be calibrated using observed discharge but due to deficiency of observed data the parameters have been adopted by engineer's empirical sense. Storage constant in the Clark unit hydrograph method mainly affects magnitude of peak flood. This study is to estimate the storage constant based on the observed rainfall-runoff data at the three stage stations in the Imjin river basin and the three stage stations in the Ansung river basin. In this study four methods have been proposed to estimate the storage constant from observed rainfall-runoff data. The HEC-HMS model has been adopted to execute the sensitivity of storage constant. A criteria has been proposed to determine storage constant based on the results of the observed hydrograph and the HEC-HMS model.

• Journal of Environmental Science International
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• v.23 no.4
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• pp.533-541
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• 2014

The streams in Jeju Island have very distinctive hydrological and geological properties and there are a lot of limits in applying the general flood estimation method. This study presented parameters dominant in the Hancheon stream of Jeju Island by analyzing the sensitivity of parameters of HEC-HMS model regarding rainfall events in the target basin, and extracted the optimal parameter(Time of Concentration of Clark Unit Hydrograph: Kraven II method, Storage Coefficient: Sabol method) by analyzing and comparing it with the flood runoff data observed in the site and Jeju Island's observation data.

• Korean Journal of Remote Sensing
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• v.23 no.1
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• pp.15-20
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• 2007

This study is to apply QuickBird satellite image for the simulation of storm runoff in a small rural watershed. For a $1.05km^2$ watershed located in Goesan-Gun of Chungbuk Province, the land use from the QuickBird image was produced by on-screening digitising after ortho-rectifying using 2 m DEM. For 3 cases of land use, soil and elevation scale (1:5,000, 1:25,000 and 1:50,000), SCS-CN and the watershed physical parameters were prepared for the storm runoff model, HEC-HMS (Hydrologic Modelling System). The model was evaluated for each case and compared the simulated results with couple of selected storm events.

• Water for future
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• v.42 no.11
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• pp.34-41
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• 2009

• Proceedings of the Korea Water Resources Association Conference
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• 2002.05b
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• pp.867-872
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• 2002

• Proceedings of the Korea Water Resources Association Conference
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• 2004.05b
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• pp.1122-1126
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• 2004

최근 기상이변과 예측을 불허하는 여러 자연현상의 변화들로 인하여 여러 가지 자연재해가 매년 늘어나는 실정이다. 이러한 자연재해 중 우리나라에서는 집중호우에 의한 홍수피해가 자주 발생하고 있으며 이를 규명하는 기법 중 최근에 많이 사용하는 GIS는 유역에서의 지형학적, 기후학적 특성을 시간과 인력에 대하여 정량화 할 수 있는 장점을 가지고 있어 점점 그 사용 추세가 증가하고 있다. 본 연구에서는 GIS를 이용한 HEC-GeoHMS와 HEC-HMS를 이용하여 판운 지점의 유출량을 예측하여 평창강 유역의 유출을 분석하였고 모형의 적용성을 검증하기 위해 단위도에 따라 SCS, Snyder, Clark 3가지 모델로 구분하여 적용에 대한 검증을 실시하고자 하였다.