• Journal of Korea Water Resources Association
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• v.32 no.4
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• pp.437-445
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• 1999

The present paper describes the problem of hydrologic response estimation using non-parametric ridge regression method. The method adapted in this work is based on the minimization of the $C_L$ statistics, which is an estimate of the mean square prediction error. For this method, effects of using both the identity matrix and the Laplacian matrix were considered. In addition, we evaluated methods for estimating the error variance of the impulse response. As a result of analyzing synthetic and real data, a good estimation was made when the Laplacian matrix for the weighting matrix and the bias corrected estimate for the error variance were used. The method and procedure presented in present paper will play a robust and effective role on separating hydrologic response.

• Water for future
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• v.23 no.4
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• pp.421-434
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• 1990

The problems of hydrologic similarity among river basins was analyzed by a geomorphologic response model using Hortons*s ordering scheme. The Nash model was used for deriving the geomorphologic response function, and for the optimization of the responsefunction, imcomplete gamma function andRosso*s regression equation were used. The application of this method was tested on some observed flood data of Pyungchang river basin and Wi Stream basin and Bocheong stream, and predictions of hydrologic response were compared with that of the Moment method. The results show that the proposed model and dimensionless instantaneous unit hydrograph can be used for the runoff analysis of an ungauged basin and the analysis of hydrologic similarity.

• Journal of Korean Society for Geospatial Information Science
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• v.18 no.2
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• pp.69-78
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• 2010

The hydrological-geomorphic character is closely related with runoff in basin. A development of GIS greatly helps investigating about mechanism between theirs. We analyze local slope and hillslope length which are related with hydrological response. But variation of these geomorphic variables has very wide range at each pixel. So there's a limit as to use directly. Therefore we investigate a relation between hydrological response and distributed geomorphic variables according to statistical character of distributed map considering spatial correlation. As a result, the local slope affects peak discharge, and the hillslope length affects peak discharge and time, mean and variance of hydrological response. Henceforth these hydrological-geomorphic analyze methods can be improved that hydrology response is directly analogized with DEM data.

• Proceedings of the Korea Water Resources Association Conference
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• 2007.05a
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• pp.1573-1577
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• 2007

SWAT 모형을 사용하여 수문 및 환경인자들의 예측에 있어서 수문응답단위(Hydrological Response Unit, HRU) 수를 적절하게 결정하는 것은 매우 중요하다. SWAT 모형에서는 수문응답단위라는 계산단위를 통하여 모형의 입력매개변수를 생성하고 모의를 수행하기 때문이다. 본 연구에서는 SWAT모형에서 하천유역의 적절한 HRU 수를 결정하기 위하여 대상유역을 낙동강의 제 1지류이자 국제수문개발계획(International Hydrologic Project, IHP)의 국내 대표유역 중 하나인 위천유역으로 선정하였으며, 토지이용과 토양의 면적비를 조정함으로써 HRU 수를 여러 단계로 적용하여 유출량, 유사량 및 영양염류를 모의하였다. SWAT 모형의 적용을 위하여 위천 유역의 $DEM(30m{\times}30m)$, 토지이용도(1:25,000), 토양도(1:25,000) 등의 GIS 자료와 강우량 및 기상자료를 이용하였다. 본 논문은 위천 유역에 대한 적절한 HRU 수의 기준을 제시하였으며, 이와 같은 분석결과를 이용하여 모형의 입력자료 구축시간을 단축할 수 있어 차후 모형의 적용시에 모형의 적용 효율을 높일 수 있을 것으로 판단된다.

• Water for future
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• v.28 no.4
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• pp.185-194
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• 1995

The objective of this study is to explore scale problem and to analyze the relations between scale and geomorphologic parameters of the rainfall-runoff model. Generally, measurement and calculation of geomorphologic parameters rely on and are sensitive to the resolution of source information available. Therefore, rainfall-runoff models using geomorphologic parameters should take account of the effects of the map scale used in their development. The derived rainfall-runoff model considering scale problem in this research is the GIUH type model, that is a basin IUH consisting of the channel network response and hillslope response. The cannel network response is computed by means of the diffusion analogy transformed from linearized St. Venant equation and hillslope response is calculated by 2-parameter gamma distribution function. Representing geomorphologic structure of the channel network and initial distribution of its response is width function. This width function is derived by fractal theory and Melton's law to consider scale problems and is weighted by the source location function (SLF) proposed in this research to increase the applicability.

• Proceedings of the Korea Water Resources Association Conference
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• 2004.05b
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• pp.1042-1046
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• 2004

본 연구는 국내 실무에서 사용되고 있는 유역응답시간 산정식의 적용성을 검토하기 위하여 기존의 8개의 도달시간 산정식과 6개의 지체시간 산정식을 유역면적이 $50\~500km^2$인 중규모유역에 적용하였으며, 실측수문 자료로부터 두가지 정의에 의해 산정한 도달시간과 지체시간을 비교, 검토하였다. 기존의 도달시간 산정식에 의한 도달시간은 실측 도달시간에 비해 모든 대상유역에서 과소한 값을 나타내었으며, 지체시간 산정식의 경우 Clark 공식과 SCS 공식은 모든 대상유역에서 과소한 값을 나타내었고 Snyder 공식, Linsley 공식, Eagleson 공식, Rao와 Delleur 공식은 대상유역에 따라 과다 또는 과소한 경향을 나타내었다. 따라서 실측수문자료에서 산정된 유역응답시간과 기존의 산정식에서 결정된 값들이 상이하게 나타나 중규모유역에서 기존의 유역응답 시간 산정식의 적용성이 떨어진다고 판단되었다. 대상유역에서 적합한 유역응답시간 공식을 유도하기 위하여 유역응답시간과 유역특성인자간의 회귀분석을 실시하였으며, 국내 중규모유역에서 적용할 수 있는 도달시간과 지체시간 산정식을 제안하였다.

• Journal of Korea Water Resources Association
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• v.30 no.2
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• pp.97-106
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• 1997

Parameters of the Nash model were analyzed using similarity concepts for the hydrogeomorphologic and the time response characteristics, then the application of parameter estimation was performed for a basin where no data are available. The self-similarity was investigated to evaluate the similarity of hydrogeomorphologic characteristics and to derive a equation for the time of concentration. The relation between model parameters and time characteristics such as travel and lag time, were developed to obtain their properties of similarity. There were remarkable results about the assessment for basin similarity and the application to an ungaged basin in Wi stream basin.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.10 no.1
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• pp.99-108
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• 1990

A Synthetic Unit Hydrograph Method was investigated for representation of the effective rainfall-direct runoff hydrograph by using a Geomorphologic Instantaneous Unit Hydrograpb(GIUH) proposed by Gupta et al(1980). The response function of the basin was assumed to be the two-parameter gamma probability density function. The physical parameters of the response function(Nash Model) was determined by using the regression eqs. were parameterized in terms of Horton order ratios and the relations between the basin lag time and time-scale parameter. The capability of the Synthetic Unit Hydrograph to the real basin was tested for the Pyungchang river basin and Wi Stream basin, and its capability to reproduce the hydrologic response was investigate and compared with the Moment Method and the Least Square Method used incomplete gamma function. The representation of the peak flow, the time to peak and the hydrographs the derived Synthetic Unit Hydrograph were tested on some obseved flood data and showed promising, and it was approved to be used for prediction of the ungaged basins.

• Proceedings of the Korea Water Resources Association Conference
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• 2010.05a
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• pp.1174-1178
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• 2010

확산-유추를 기반으로 한 지형학적 순간단위도의 유역의 동역학적 매개변수인 특성유속과 확산계수를 실제수문사상과 수치지형도상의 실제 하천망(Blue line)을 이용해 전역최적화 기법인 Shuffled Complex Evolution(SCE-UA)을 적용하여 산정하여 이를 하천망의 해상도에 따른 유역의 수문응답의 특성을 살펴본 결과 동일한 산정된 유속조건하에서 하천망의 해상도가 커짐에 따라 첨두시간과 지체시간은 작아지는 반면 첨두유량은 커지는 현상을 보였으며, 순간단위도의 형상을 결정짓는 유하시간 분포의 분산은 동수역학적 분산에 비해 지형학적 분산에 지배적인 영향을 받음을 알 수 있었다.

• Journal of Korean Society for Geospatial Information Science
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• v.20 no.1
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• pp.13-20
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• 2012

In this study, the change pattern of hydrological response function as development has been observed. The target watershed was selected Tanbu sub-Basin in the Bocheong Basin. The applied channel networks are composed of 10 cases that are channel networks by strahler's ordering scheme and cases of all grids channel or the hillslope in basin. To each case of grid in basin, channel and hillslope drainage path lengths to outlet of basin are calculated, and hydrological response function was calculated by Nash Model. As results of this analysis, the peak discharge of hydrological response function is increased and peak time is shortened as development of channel networks. And based on statistical characteristics of hydrological response function, mean (lag time) and variance of travel time are reduced exponentially.