• Proceedings of the Korea Water Resources Association Conference
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• 1993.07a
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• pp.293-300
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• 1993

• Proceedings of the KSEEG Conference
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• 2002.04a
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• pp.91-91
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• 2002

• Journal of Korea Water Resources Association
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• v.40 no.4
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• pp.299-311
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• 2007

Climatic abnormal phenomena involving El Nino and La Nina have been frequently reported in recent decades. The interannual climate variability represented by El Nino-Southern Oscillation (ENSO) is sometimes investigated to account for the climatic abnormal phenomena around the world. Although many hydroclimatologists have studied the impact of ENSO on regional precipitation and streamflow, however, there are still many difficulties in finding the dominant causal relationship between them. This relationship is very useful in making hydrological forecasting models for water resources management. In this study, the seasonal relationships between ENSO and hydrologic variables were investigated in Korea. As an ENSO indicator, Southern Oscillation Index (SOI) was used. Monthly precipitation, monthly mean temperature, and monthly dam inflow data were used after being transformed to the standardized normal index. Seasonal relationships between ENSO and hydrologic variables were investigated based on the exceedance probability and distribution of hydrologic variables conditioned on the ENSO episode. The results from the analysis of this study showed that the warm ENSO episode affects increases in precipitation and temperature, and the cold ENSO episode is related with decreases in precipitation and temperature in Korea. However, in some regions, the local relationships do not correspond with the general seasonal relationship.

• Water for future
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• v.18 no.2
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• pp.153-161
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• 1985

The methods for hydrologic prediction of streamflows for more efficient and functional operations and automation of the flood warning and forecasting system have been studiedand which have been widely used in the control engineering have been studied and investigated for representation of the dynamic behavior of rainfall-runoff precesses, and formulated into mathematical model form. The applicabilities of the model using the adaptive Kalman filter algorithm to the on-line, real-time prediction of river flows have been worked out. The computer programs in FORTRAN which are developed here can be utilized for more efficient operations and better prediction abilities of flood warning and forecasting systems, and also should be modified for better model performance.

• Proceedings of the Korea Water Resources Association Conference
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• 2004.05b
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• pp.1267-1270
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• 2004

DEM(Digital Elevation Model)을 활용한 기술이 수자원분야에서 필수적인 GIS 활용기술인 이유는 DEM을 이용할 경우 유역의 수문학적 지형특성인자를 객관적인 방법으로 추출할 수 있고 이를 활용하여 분포형 수문모형을 개발, 적용할 수 있기 때문이다. 국내에서도 GIS를 이용하여 수문모형의 입력인자를 추출한 다든가 분포형 수문모형에 대한 연구를 수행할 경우 DEM을 활용한 연구를 수행하고 있다. 이러한 것은 GIS S/W인 Arc/Info, ArcView, WMS 등에서 DEM을 활용하여 수문학적인 유역분석 기능을 제공해 주기 때문에 가능하다. 즉, DEM을 이용하여 하천망을 추출하고, 유역을 분한하고 이를 이용하여 유역 Boundary 내에서의 지형특성인자를 추출하는 기능을 말한다 본 연구는 수자원분야에서 GIS를 활용할 때 필요한 필수기능인 DEM의 활용기술을 순수 국내기술로 개발하였다. DEM활용에 대한 최신 알고리즘을 검토하여 국내 기술로 개발된 GIS Engine인 GEOMaina v.3.0을 이용하여 수문학적인 DEM 활용 Module을 개발하였으며 HyGIS(Hydrologic Geography Information System)라 명하였다. 본 연구에서는 개발된 HyGIS를 이용하여 수문학적 지형특성인자를 추출하고 기존에 사용되어오던 GIS S/W와 비교 검토하여 HyGIS의 환용 가능성에 대하여 검토하고자 한다.

• Proceedings of the Korea Water Resources Association Conference
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• 2012.05a
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• pp.641-641
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• 2012

하천관련 정보관리기술의 발전을 위해서는 관련자료 출처 발굴과 자료의 통합관리 및 분석 기술개발 등의 노력이 필요하다. 이에 따라 하천관련 정보에 대한 관리기술의 선진사례 분석을 통하여 국외의 앞선 기술을 살펴보고 국내 적용 방안을 제시하고자 한다. 본 연구에서 분석한 미국의 HIS (Hydrologic Information System)는 CUAHSI (Consortium of Universities for the Advancement of Hydrologic Science, Inc)에서 수행하는 연구 활동의 하나로서 개방형 프로젝트로 개발되고 있으며 수문분석에 필요한 정보를 통합하여 관리하고 배포하는 기능을 수행하고 있다. CUAHSI-HIS는 웹기반 시스템이며 HIS 중심부(데이터 목록), Hydro 서버(데이터 게시), HydroDesktop (사용자 검색툴)으로 구성되어 있다. 이 세 개의 핵심 요소들은 상호작용을 통해 운영되며 미국 내의 모든 물관련 자료를 발굴하고 수집한다. 이렇게 발굴 수집된 자료는 WaterML로 표준화하여 다양한 사용자가 쉽게 사용할 수 있도록 제공된다. 국내의 경우 RIMGIS와 WAMIS 등이 하천정보를 제공하고 있지만 변화된 하천운영 환경을 반영하여 사용자에게 보다 체계적이고 효율적인 정보를 제공하기 위해서는 정보의 표준화 및 시스템 구성환경 등 다양한 측면에서 검토가 필요하다. 이를 위해 CUAHSI-HIS 연구사례를 벤치마킹하여 국내 실정에 맞는 적용방안을 수립하여 구축하게 된다며 체계적인 정보관리 및 활용성을 극대화할 수 있을 것으로 사료된다.

• Journal of Korean Society on Water Environment
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• v.23 no.4
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• pp.535-542
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• 2007

The Geumho river watershed located in the middle of the Nakdong river has been threatened by high population growth and urbanization. Of concern specifically is the potential impact of future developments in the watershed on the reduction of base flow and the consequent risk of degradation of ecological habitats in Geumho river. Anticipated increase in imperviousness, on the other hand, is expected to elevate flood risk and the associated environmental damage. A watershed hydrology based modeling study is initiated in this study to assist in planning for sustainable future development in the Geumho river watershed. The Soil and Water Assessment Tool (SWAT) is selected to model the impact of urbanization in the Geumho river watershed on the hydrologic response thereof. The modeling results show that in general the likelihood that the watershed will experience high and low stream flows will increase in view of the urbanization so far achieved.

• Korean Journal of Remote Sensing
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• v.24 no.1
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• pp.25-33
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• 2008

To investigate the hydrologic impacts of climate changes on dam inflow for Soyanggangdam watershed $(2694.4km^2)$ of northeastern South Korea, SLURP (Semi-distributed Land Use-based Runoff Process) model and the climate change results of CCCma CGCM2 based on SRES A2 and B2 were adopted. By the CA-Markov technique, future land use changes were estimated using the three land cover maps (1985, 1990, 2000) classified by Landsat TM satellite images. NDVI values for 2050 and 2100 land uses were estimated from the relationship of NDVI-Temperature linear regression derived from the observed data (1998-2002). Before the assessment, the SLURP model was calibrated and verified using 4 years (1998-2001) dam inflow data with the Nash-Sutcliffe efficiencies of 0.61 to 0.77. In case of A2 scenario, the dam inflows of 2050 and 2100 decreased 49.7 % and 25.0 % comparing with the dam inflow of 2000, and in case of B2 scenario, the dam inflows of 2050 and 2100 decreased 45.3 % and 53.0 %, respectively. The results showed that the impact of land use change covered 2.3 % to 4.9 % for the dam inflow change.

• Journal of The Korean Society of Agricultural Engineers
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• v.65 no.1
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• pp.41-49
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• 2023

To utilize the hydraulic and hydrological models when simulating floods in agricultural watersheds, it is necessary to consider agricultural reservoirs, farmland, and farmland drainage system, which are characteristics of agricultural watersheds. However, most of them are developed individually by different researchers, also, each model has a different simulation scope, so it is hard to use them integrally. As a result, there is a need to link each hydraulic and hydrological model. Therefore, this study established an integrated flood simulation system for the comprehensive flood simulation of agricultural reservoir watersheds. The system can be applied easily to various watersheds because historical weather data and the SSP (Shared Socio-economic Pathways) climate change scenario database of ninety weather stations were built-in. Individual hydraulic and hydrological models were coded and coupled through Python. The system consists of multiplicative random cascade model, Clark unit hydrograph model, frequency analysis model, HEC-5 (Hydrologic Engineering Center-5), HEC-RAS (Hydrologic Engineering Center-River Analysis System), and farmland drainage simulation model. In the case of external models with limitations in conceptualization, such as HEC-5 and HEC-RAS, the python interpreter approaches the operating system and gives commands to run the models. All models except two are built based on the logical concept.

• Journal of Korea Water Resources Association
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• v.37 no.5
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• pp.407-424
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• 2004

Using geomorphoclimatic unit hydrograph(GCUH), we estimated the fitness to calculate the mountainous area discharge and flash flood trigger rainfall(FFTR). First, we compared the GCUH peak discharge with the existing report using the design storm at the Dukcheon basin. Second, we compared the HEC-HMS(Hydrologic Engineering Center-Hydrologic Modeling System) model and GCUH with the observed discharge using the real rainfall events at the Taesu stage gage. Third, GCUH and NRCS(Natural Resources Conservation Service) were used for calculating FFTR and proper calculation method was shown. At the Dukcheon basin, the comparison result of using design storm was shown in Table 11, and it was not in excess of 1.1, except for the 30 year return period. In case of real rainfall events, the result was shown in Table 12, and GCUH discharges were all larger than the HEC-HMS model discharges, and they were very similar to the observed data at the Taesu stage gage. In this study, we found that GCUH was a very proper method in the calculation of mountainous discharge. At the Dukcheon basin, FFTR was 12.96 mm in the first 10 minutes when the threshold discharge was 95.59 $m^3$/sec.