• 한국환경과학회지
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• 제1권2호
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• pp.105.2-117
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• 1992

The formation mechanism of the vortex streets in the lee of the mountain Is Investigated by a three-dimensional numerical model. The model is based upon the hydrostatic Boussinesq equations in which the vertical turbulent momentum flux is estimated by a turbulence parameterization scheme, but the horizontal viscosity is assumed to be constant. The results show that Karman vortex streets can form even without surface friction in a constant ambient flow with uniform stratification. The vortex formation is related to breaking of the mountain wave, which depends on the Froude number (Fr). In the case of a three-dimensional bell-shaped mountain, the wave breaking occurs when Fr is less than about 0.8, while a barman vortex forms when Fr is less than about 0.22. Vortex formation also depends on Reynolds number, which is estimated from the horizontal diffusivity. The vortex formation can be explained by the wave saturation theory given by Lindzen (1981) with some modification. Simulations in this study show that in the case of Karman vortex formation the momentum flux in the lower level is much larger than the saturated momentum flux, whereas it is almost equal to the saturated momentum at the upper levels as expected from the saturation theory. As a result, large flux divergence is produced in the lower layer, the mean flow is decelerated behind the mountain, and the horizontal wind shear forms between unmodified ambient wind. The momentum exchange between the mean flow and the mountain wave is produced by the turbulence within a breaking wave. From the result, well developed vortices like Karman vortex can be formed. . The results of the momentum budget calculated by the hydrostatic model are almost the same as nonhydrostatic results as long as horizontal scale of the mountain is 10 km. A well developed barman vortex similar to the hydrostatic one was simulated in the nonhydrostatic case. Therefore, we conclude that the hydrostatic assumption is adequate to investigate the origin of the Km8n vortex from the viewpoint of wave breaking.

• 재무관리연구
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• 제23권2호
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• pp.1-25
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• 2006

본 논문에서는 1980년부터 2003년까지 한국 증권시장을 대상으로 과거 주식수익률과 변동성을 이용한 반대투자전략의 초과수익을 분석하였다. 즉 과거 주식수익률을 이용한 투자전략의 초과수익에 시장변동성이나 개별기업의 변동성이 영향을 미치는지 검증하고자 하였다. 우선 한국 증권시장을 6년 단위의 하위 포트폴리로 구분하여 과거 주식수익률을 이용한 반대투자전략의 초과수익을 측정하였다. 그 결과 시장변동성이 가장 작은 기간이었던 1980년${\sim}$1986년까지의 표본기간에서는 계속투자전략이 유의한 투자전략으로 나타났으나 그 외의 기간에서는 반대투자전략이 유의한 투자전략으로 나타났다. 따라서 시장변동성 뿐 아니라 개별기업의 변동성 역시 과거 주식수익률을 이용한 투자전략의 초과수익에 영향을 미치는지 확인하였다. 개별기업의 변동성을 하나의 지표로 포트폴리오를 구성하여 과거 주식수익률을 이용한 투자전략의 초과수익을 확인한 결과 과거 개별기업의 변동성이 작았던 포트폴리오에서는 계속투자전략이 유의한 투자 전략으로 나타난데 비해서 과거 개별기업의 변동성이 큰 포트폴리오에서는 유의한 계속투자전략의 초과수익을 확인할 수 없었다. 따라서 과거 주식수익률 뿐 아니라 변동성까지 고려하여 투자전략을 구성하는 것이 보다 높은 양(+)의 초과수익을 얻는 방법이라고 할 수 있다.

• Environmental Sciences Bulletin of The Korean Environmental Sciences Society
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• 제1권2호
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• pp.105-117
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• 1997

The formation mechanism of the vortex streets in the lee of the mountain is investigated by a three-dimensional numerical model. The model is based upon the hydrostatic Boussinesq equations in which the vertical turbulent momentum flux is estimated by a turbulence parameterization scheme, but the horizontal viscosity is assumed to be constant. The results show that Karman vortex streets can form even without surface friction in a constant ambient flow with uniform stratification. The vortex formation is related to breaking of the mountain wave, which depends on the Froude number (Fr). In the case of a three-dimensional bell-shaped mountain, the wave breaking occurs when Fr is less than about 0.8, while a Karman vortex forms when Fr is less than about 0.22. Vortex formation also depends on Reynolds number, which is estimated from the horizontal diffusivity. The vortex formation can be explained by the wave saturation theory given by Lindzen (1981) with some modification. Simulations in this study show that in the case of Karman vortex formation the momentum flux in the lower level is much larger than the saturated momentum flux whereas it is almost equal to the saturated momentum at the upper levels as expected from the saturation theory. As a result, large flux divergence is produced in the lower layer, the mean flow is decelerated behind the mountain, and the horizontal wind shear forms between unmodified ambient wind. The momentum exchange between the mean flow and the mountain wave is produced by the turbulence within a breaking wave. From the result, well developed vortices like Karman vortex can be formed. The results of the momentum budget calculated by the hydrostatic model are almost the same as nonhydrostatic results as long as horizontal scale of the mountain is 10 km. A well developed Karman vortex similar to the hydrostatic one was simulated in the nonhydrostatic case. Therefore, we conclude that the hydrostatic assumption is adequate to investigate the origin of the Karman vortex from the viewpoint of wave breaking.

• 한국항공우주학회지
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• 제37권2호
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• pp.113-120
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• 2009

로터-기체 사이의 간섭작용을 정확하게 계산하기 위해서는 로터의 회전을 사실적으로 모사할 수 있는 로터-기체 결합형상의 Navier-Stokes 해석이 필요하다. 하지만 회전하는 로터를 포함한 전기체를 해석할 경우 격자가 증가함에 따라 계산 비용과 시간이 증가된다. 모멘텀 소스 방법은 로터를 디스크 격자에 모멘텀 소스로 대체하여 시간 평균된 로터-기체의 간섭작용을 해석하므로 비교적 경제적이면서도 정확한 결과를 얻을 수 있다. 일반적으로 모멘텀 소스 값은 블레이드 요소 이론을 이용하여 구하지만 결과의 정확성이 떨어진다. 따라서 본 연구에서는 모멘텀 소스를 Moving mesh 방법을 이용한 Navier-Stokes 계산을 통해 구하여 정확성을 높였다. 이 모멘텀 소스 값을 이용하여 정상해석을 하여 실험결과와 비교하였다. 기존의 모멘텀 소스 방법은 시간 평균된 유동장만 관찰할 수 있으므로 비정상 유동장을 관찰하기 위하여 비정상 로터-기체 간섭작용 해석 모델을 개발하여 실험결과와 비교해 보았다. 검증을 위하여 간단한 형상인 Georgia Tech 형상을 사용하여 실험결과와 비교해 보았으며 본 연구의 계산결과가 실험결과와 잘 일치하는 것을 볼 수 있었다.

• 대한기계학회:학술대회논문집
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• 대한기계학회 2005년도 창립60주년 기념 추계 학술대회
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• pp.60.2-60.2
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• 2005

• 한국운동역학회지
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• 제17권4호
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• pp.83-88
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• 2007

The purpose of this study was to investigate the ball velocity changes depending on the different linear momentum of putter head. For this study, two different moving conditions(25cm free fall and 35cm free fall) of putter head were set. And two different types of ground conditions were used which are artificial grass green($180cm{\times}600cm{\times}1cm$) and glass green($40cm{\times}130cm{\times}1cm$). Movements of putter head and ball were recorded with 2 HD video cameras(60 Hz, 1/500s shutter speed). Small size control object($18.5cm{\times}18.5cm{\times}78.5cm$) was used in this study. Ball and putter head velocities were calculated by the First Central Difference Method(Hamill & Knutzen, 1995). Linear momentum of ball and putter head were calculated with mass and its velocities. Before impact, the velocity of the putter head of 35cm free fall was about 30% greater than that of the putter head of 25cm free fall. Linear momentum of putter head of 35cm free fall was about 0.355-0.364kg m/s and 25cm free fall was 0.251 kg m/s. After impact, putter head lost its linear momentum about 14-19% and adjusting time of putter head after impact would be 0.1 second. After 0.1 second, putter moved the route same as before impact. Maximum ball velocities were appeared 0.08s-0.10s after impact no matter what the ground conditions are. Ball velocities struck by 35cm free fall were 30 % faster than 25cm free fall. Linear momentum of ball struck by putter head was greater than that of expected amount because the moving ball has translational energy and rotational energy. Future study must treat three things. One is ball must struck by the different putters with different materials. Another is two-piece ball and three-piece ball should be used for the same condition studies. The other is height of center of rotation of club should be changed. In this study, the height of center of rotation of club head is 71cm from the ground. But recently many golfers used the long putter. Therefore next study should apply the different height of center of rotation of club head.

• 한국수소및신에너지학회논문집
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• 제16권1호
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• pp.1-8
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• 2005

Transition of momentum-controlling hydrogen jet to buoyant jet is experimentally investigated in order to develop a prediction model for the moving trajectory of hydrogen leaked from hydrogen devices. In the experiments, room-temperature helium, that has a similar density to the hydrogen leaked from high pressure tank, is horizontally injected through a 4mm tube and its moving trajectory is visualized by the shadowgraph method. The moving trajectories are found to be parabolic, thereby exhibiting increasing influence of the buoyancy. In analyzing the experimental results, the vertical movement is assumed to be controlled by the buoyancy while the horizontal movement is controlled by the air entrainment caused by the initial momentum. The resealing based on this assumption yields a single curve fitting to the all experimental results.

• 디자인학연구
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• 제20권3호
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• pp.39-48
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• 2007

본 논문은 도시환경의 공공사인시스템의 효율극대화를 위하여 안구운동을 측정하는 공학 심리적 또는 인지 과학적 실험을 통하여 안구운동과 가로세로의 시각흐름 그리고 유전된 문화적. 선험적 도식 그리고 대뇌의 시각 시스템의 차별을 탐색하였다. 따라서 EMR 관측실험과 bitmap counting 방법을 대입함으로서 가장 효율적인 시각디자인 측정을 구할 수 있는 algorithm을 도출하였다. 본 논문에서는 과학적인 실험 Data가 인간의 $\ulcorner$Schema$\lrcorner$ 와 $\ulcorner$Sensory Qualia$\lrcorner$ 에 의해, 차별화와 시각표집(Visual Sampling)의 가변성(Momentum)이 상존함을 알게 되었다.

• 천문학회지
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• 제44권2호
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• pp.49-58
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• 2011

We calculate the energy spectra of cosmic ray (CR) protons and electrons at a plane shock with quasi-parallel magnetic fields, using time-dependent, diffusive shock acceleration (DSA) simulations, including energy losses via synchrotron emission and Inverse Compton (IC) scattering. A thermal leakage injection model and a Bohm type diffusion coefficient are adopted. The electron spectrum at the shock becomes steady after the DSA energy gains balance the synchrotron/IC losses, and it cuts off at the equilibrium momentum $p_{eq}$. In the postshock region the cutoff momentum of the electron spectrum decreases with the distance from the shock due to the energy losses and the thickness of the spatial distribution of electrons scales as $p^{-1}$. Thus the slope of the downstream integrated spectrum steepens by one power of p for $p_{br}$ < p < $p_{eq}$, where the break momentum decreases with the shock age as $p_{br}\;{\infty}\;t^{-1}$. In a CR modified shock, both the proton and electron spectrum exhibit a concave curvature and deviate from the canonical test-particle power-law, and the upstream integrated electron spectrum could dominate over the downstream integrated spectrum near the cutoff momentum. Thus the spectral shape near the cutoff of X-ray synchrotron emission could reveal a signature of nonlinear DSA.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 1992년도 수공학연구발표회논문집
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• pp.55-66
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• 1992

수로단면의 유속분포가 균일하지 않으므로, 에너지 원리의 $\alpha$값과 운동량원리의 $\beta$값 각각에 미치나, 대부분 실무에서는 이들 값을 추정하는 어려움 때문에 통상 1로 가정하여 사용하고 있다. 본 연구에서는 실용적으로 이용할 수 있는 공식을 유도하고, 기존에 사용되고있는 Prandtl-Von Karman 공식과 비교 검토하였으며, 유속분포계수 공식을 유도하기 위하여, 수로 바닥과 수 표면까지도 포함한 전 영역에서 비교적 정확한 유속분포를 나타내는 Chiu의 유속공식을 사용하였다. 또한, 실용적목적을 위해 유속데이타 없이 유속분포 계수를 구하기 위해서 Manning공식과 Chiu공식을 사용하였으며, 실험실 및 현장데이타를 위의 연구에 적용 검증하였다.