• 한국농공학회지
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• 제37권3_4호
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• pp.34-47
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• 1995

It is experienced fact as a regular annual event that the structure to he designed on unreasonable flood for the agricultural structures including reservoirs have been brought not only loss of lives, but also enormous property damage. For the solution of this problem at issue, this study was conducted to develop an optimal runoff hydrograph model by comparison of the peak flows and time to peak between observed and simulated flows derived by linear time-invariant and linear time-variant models under the condition of having a short duration of heavy rainfall with uniform rainfall intensity at nine small watersheds which are within the range of 55.9 to 140.7 square kilometers in area in Han, Geum, Nagdong and Yeongsan Rivers. The results obtained through this study can be summarized as follows. 1. Storage constants and Gamma function arguments were calculated within the range of 1.2 to 6.42 and of 1.28 to 8.05 respectively by the moment method as the parameters for the analysis of runoff hydrograph based on linear time-invariant model. 2. Parameters for both linear time-invariant and linear time-variant models were calibrated with nine gaged watershed data, using a trial and error method. The resulting parameters including Gamma function argument, N and storage constant, K for linear time-invariant model were related statistically to watershed characteristic variables such as area, slope, length of main stream and the centroid length of the basin. 3. Average relative errors of the simulated peak discharge of calibrated runoff hydrographs by using linear time-variant and linear time-invariant models were shown to be 0.75 and 5.42 percent respectively to the peak of observed runoff hydrographs. Correlation coefficients for the statistical analysis in the same condition were shown to be 0.999 and 0.978 with a high significance respectively. Therefore, it can be concluded that the accuracy of a linear time-variant model is approaching more closely to the observed runoff hydrograph than that of a linear time-invariant model in the applied watersheds. 4. Average relative errors of the time to peak of calibrated runoff hydrographs by using linear time-variant and linear time-invariant models were shown to be 16.44 and 19.89 percent respectively to the time to peak of observed runoff hydrographs. Correlation coefficients in the same condition were also shown to be 0.999 and 0.886 with a high significance respectively. 5. It can be seen that the shape of simulated hydrograph based on a linear time- variant model is getting closer to the observed runoff hydrograph than that of a linear time-invariant model in the applied watersheds. 6. Two different models were verified with different rainfall-runoff events from data for the calibration by relative error and correlation analysis. Consequently, it can be generally concluded that verification results for the peak discharge and time to peak of simulated runoff hydrographs were in good agreement with those of calibrated runoff hydrographs.

• 대한전자공학회논문지SP
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• 제46권2호
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• pp.89-98
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• 2009

컴퓨터 비전 분야에서 영상 모자이킹 (Image Mosaicking)은 제한된 시야각의 카메라를 사용하여 획득한 여러 장의 중첩된 영역을 가지는 영상을 한 장의 영상으로 정합하여 나타내는 기법이다. 최근에는 연속된 영상에서 카메라의 기학학적인 움직임 때문에 발생하는 영상의 왜곡이나 밝기 차에 관계없이 정확한 정합을 수행하기 위해서 특징점을 기반으로 서술자를 구성하는 정합 방법이 많이 연구되고 있다. 그러나 대부분의 특징점 검출 알고리즘들은 영상의 밝기값 기반의 처리 과정을 수행하기 때문에 영상의 칼라 성분은 다르지만 밝기값이 비슷한 경우, 또는 동영상에서 시간의 흐름에 따라 광원이 변화하는 경우에는 광원의 영향에 따라 검출되는 특징점의 수와 각각의 지역 서술자의 특성이 변하여 정확한 대응점을 검출하는데 오류를 유발하게 된다. 이런 문제점을 해결하기 위해서 본 논문은 영상의 칼라 정보를 이용한 특징점 기반의 영상 모자이킹 방법을 제안하였다. 디지털 칼라 카메라로부터 획득한 디지털 값을 좁은 대역을 갖는 가상의 카메라 출력값으로 변환하여 물체의 분광 반사율 기반의 값으로 유도하고 이것을 광원의 변화에 불변하는 칼라 불변 값 (Color-Invariant Value)으로 정의하였다. 제안된 칼라 불변값의 유효성을 검증하기 위해서 시뮬레이션된 광원들과 Macbeth Color-Checker를 이용하여 확인하였으며, 실험결과에서 제안한 방법과 기존의 SIFT 알고리즘을 비교를 통해 제안된 방법의 정합율의 향상을 확인하였다.

• Korean Journal of Mathematics
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• 제9권2호
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• pp.149-156
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• 2001

We characterize some properties of $t$-fuzzy groups and $t$-fuzzy invariant groups and represent every subgroup S of a group X using the level set of $t$-fuzzy group constructed from S.

• 호남수학학술지
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• 제26권2호
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• pp.137-145
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• 2004

we shall study some properties of a new class ($\sqrt[\kappa]{P}$) (defined below). Also we show that T may not be normaloid when $T{\in}(\sqrt[\kappa]{P})$, and that the class ($\sqrt{H}$) may not have the translation-invariant propety.

• 대한전자공학회:학술대회논문집
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• 대한전자공학회 2004년도 학술대회지
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• pp.897-899
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• 2004

There is scientific work containing the recurrence method of synthesis the new class of orthogonal circle m-invariant signals: designed effective algorithms of fast-direct computing m-convolution in time domain: engineer methods of design economic scheme of decoders for optimal receiving in aggregate of suggested signal.

• 대한수학회논문집
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• 제11권4호
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• pp.1055-1059
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• 1996

We characterize the left invariant Riemannian metrics on SO(1,2) which give rise to 3- or 4-dimensional isometry groups.

• Journal of the Korean Statistical Society
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• 제18권1호
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• pp.62-71
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• 1989

We consider a Markov proces ${X_n} on [0,\infty)^k$ which is generated by $X_{n+1} = f(X_n) + \varepsilon_{n+1}$ where f is a continuous, nondecreasing concave function. Sufficient conditions for the existence of a unique invariant probability measure for ${X_n}$ are obtained.

• 대한수학회지
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• 제32권4호
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• pp.661-678
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• 1995

In this paper we will estimate from above and below the values of the Bergman, Caratheodory and Kobayashi metrics for a vector X at z, where z is any point near a given point $z_0$ in the boundary of pseudoconvex domains in $C^n$.

• 대한수학회논문집
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• 제10권4호
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• pp.867-874
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• 1995

Linear invariance is closely related to the concept of uniform local univalence. We give a geometric proof that a holomorphic locally univalent function defined on the open unit disk is linearly invariant if and only if it is uniformly locally univalent.

• Korean Journal of Mathematics
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• 제10권1호
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• pp.67-74
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• 2002

Suppose linear forms whose coefficients are arithmetic progressions are given. In this paper, we will find the upper and lower bounds of the minimal ranks of subforms of these forms which left the Frobenius numbers invariant. This is an improvement of Ritter's bounds.