간행물

한국수자원학회 논문집 KCI 등재 Journal of Korea Water Resources Association

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Vol. 33 No. S (2000년 12월) 161

1.
2000.12 서비스 종료(열람 제한)
A newly developed heuristic algorithm, Harmony Search, is applied to the parameter calibration problem of the nonlinear Muskingum model. The Harmony Search could, mimicking the improvisation of music player, find better parameter values for in the nonline
2.
2000.12 서비스 종료(열람 제한)
The role of river in the global water cycles and the modelling the horizontal water transport by rivers in the global scale are discussed. Due to the consolidation of the various hydrological information of the planet, now it is possible to monitor and si
3.
2000.12 서비스 종료(열람 제한)
The grid-based KIneMatic wave STOrm Runoff Model(Kim, 1998; Kim, et al., 1998) which predicts temporal variation and spatial distribution of saturated overland flow, subsurface flow and stream flow was evaluated at two watersheds. this model adopts the si
4.
2000.12 서비스 종료(열람 제한)
A TIN, Triagulated Irregular Network, based topographic modeling method and a distributed rainfall-runoff model using the topographic representation is presented. In the TIN based topographic representation, a watershed basin is modeled as a set of contig
5.
2000.12 서비스 종료(열람 제한)
The method of delays is widely used for reconstruction chaotic attractors from experimental observations. Many studies have used a fixed delay time as the embedding dimension m is increased, but this is not necessarily the best choice for obtaining good
6.
2000.12 서비스 종료(열람 제한)
In this paper, properties of hydrologic cycle in three experimental catchments were compared and different types of a lumped parametric model were applied to understand the hydrologic cycle in the catchments. One of them is a forest catchment and another
15.
2000.12 서비스 종료(열람 제한)
This paper introduces the equivalent frequency response method(EFRM) into runoff analysis. This EFRM originally had been developed to analyze dynamic behavior of nonlinear elements such as threshold and saturation in control engineering. Many runoff model
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