Abstract
시간 및 공간가중치를 고정하지 않는 Muskingum-Cunge 홍수추적방법에 대한 오차해석을 수행하였다. 오차해석 결과 시간가중치와 공간가중치의 합이 1.0이상인 경우에는 홍수파가 진행하면서 증폭되어 수치해가 발산하였다. 시간가중치와 공간가중치의 합이 작을수록 수치확산이 크게 발생하였다. 격자의 해상도가 낮을수록 수치확산 및 수치진동이 크게 발생하였다. 수치실험과 자연하천에 대한 적용 결과, 공간가중치를 고정하지 않는 경우에는 공간가중치를 0.5로 고정하는 전통적인 Muskingum-Cunge방법보다 첨두의 감쇄가 큰 홍수파 모의에 효과적임을 알 수 있었다. Error analysis of finite difference equation on the Muskingum-Cunge flood routing method with free time and space weighting factor was carried out. The error analysis shows that the numerical solution of the Muskingum-Cunge method becomes diverged with time when the sum of time weighting factor and space weighting factor is greater than 1.0. Numerical diffusion increases when the sum of time weighting factor and space weighting factor decreases. Numerical diffusion and numerical oscillation increase when the grid resolution is coarse. Numerical experiments and field applications show that the Muskingum-Cunge method with free space weighting factor is more effective for simulating the flood routing with great peak diminution than conventional Muskingum-Cunge method with fixed space weighting factor, 0.5.
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