• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2003년도 Proceedings of ACRS 2003 ISRS
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• pp.63-65
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• 2003

The purpose of the study is to produce the surface ground temperature diagnostically using surface EBM with the use of GRID model in Geographic Information Systems (GIS). Certain characteristics have been analyzed for local slope effect, coastal effect and influence of high orographic aspect on the surface ground temperature. We present discussions on the meteorological responsibility for their temperature. The derived surface ground temperatures can be provided for comparison with those from satellite-based observ ation.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2009년도 학술발표회 초록집
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• pp.529-534
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• 2009

Climate models, both global and regional, have increased in sophistication and are being run at increasingly higher resolutions. The Land Surface Models (LSMs) coupled to these climate models have evolved from simple bucket models to sophisticated Soil-Vegetation-Atmosphere Transfer (SVAT) schemes needed to support complex linkages and processes. However, some underpinnings of terrestrial hydrologic parameterizations so crucial in the predictions of surface water and energy fluxes cause model errors that often manifest as non-linear drifts in the dynamic response of land surface processes. This requires the improved parameterizations of key processes for the terrestrial hydrologic scheme to improve the model predictability in surface water and energy fluxes. The Common Land Model (CLM), one of state-of-the-art LSMs, is the land component of the Community Climate System Model (CCSM). However, CLM also has energy and water biases resulting from deficiencies in some parameterizations related to hydrological processes. This research presents the implementation of a selected set of parameterizations and their effects on the runoff prediction. The modifications consist of new parameterizations for soil hydraulic conductivity, water table depth, frozen soil, soil water availability, and topographically controlled baseflow. The results from a set of offline simulations are compared with observed data to assess the performance of the new model. It is expected that the advanced terrestrial hydrologic scheme coupled to the current CLM can improve model predictability for better prediction of runoff that has a large impact on the surface water and energy balance crucial to climate variability and change studies.

• Structural Engineering and Mechanics
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• 제44권4호
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• pp.431-448
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• 2012

In this paper, the first-order shear deformation theory (FSDT) (Mindlin) for continuum incorporating surface energy is exploited to study the static behavior of ultra-thin functionally graded (FG) plates. The size-dependent mechanical response is very important while the plate thickness reduces to micro/nano scales. Bulk stresses on the surfaces are required to satisfy the surface balance conditions involving surface stresses. Unlike the classical continuum plate models, the bulk transverse normal stress is preserved here. By incorporating the surface energies into the principle of minimum potential energy, a series of continuum governing differential equations which include intrinsic length scales are derived. The modifications over the classical continuum stiffness are also obtained. To illustrate the application of the theory, simply supported micro/nano scaled rectangular films subjected to a transverse mechanical load are investigated. Numerical examples are presented to present the effects of surface energies on the behavior of functionally graded (FG) film, whose effective elastic moduli of its bulk material are represented by the simple power law. The proposed model is then used for a comparison between the continuum analysis of FG ultra-thin plates with and without incorporating surface effects. Also, the transverse shear strain effect is studied by a comparison between the FG plate behavior based on Kirchhoff and Mindlin assumptions. In our analysis the residual surface tension under unstrained conditions and the surface Lame constants are expected to be the same for the upper and lower surfaces of the FG plate. The proposed model is verified by previous work.

• 한국원자력학회:학술대회논문집
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• 한국원자력학회 1997년도 추계학술발표회논문집(1)
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• pp.19-24
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• 1997

In this study, we extend the application of the interface-matrix(IM) method for reflector modeling to Analytic Flux Expansion Nodal (AFEN) method. This include the modifications of the surface-averaged net current continuity and the net leakage balance conditions for IM method in accordance with AFEN fomular. AFEN-interface matrix (AFEN-IM) method has been tested against ZION-1 benchmark problem. The numerical result AFEN-IM method shows 1.24% of maximum error and 0.42% of root-mean square error in assembly power distribution, and 0.006%Δk of neutron multiplication factor. This result proves that the interface-matrix method for reflector modeling can be useful in AFEN method.

• 한국환경과학회지
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• 제8권2호
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• pp.151-154
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• 1999

To verify the accuracy of the numerical experiment of Part I, measurements at the matured rice canopy located around Junam reservoir were performed at August 14, 1995. According to the measured data, the foliage temperature recorded the highest value, and the ground temperature was the lowest around noon, and these results coincided with those of the numerical experiment using the combined model of Part I. From the estimation using measured data, the maximum value of the latent heat flux was 380$Wm^2$, the highest value among energy balance terms, and the energy redistribution ratio of the latent heat flux was averaged as 0.5, the highest values among redistribution ratios. These results are the same as those of the numerical experiment in tendency, but they reveals a little lower in the absolute values than those from the numerical experiment.

• 한국환경과학회지
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• 제3권1호
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• pp.17-29
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• 1994

An one dimensional atmosphere-vegetation interaction model is developed to discuss of the effect of vegetation on heat flux in mesoscale planetary boundary layer. The canopy model was a coupled system of three balance equations of energy, moisture at ground surface and energy state of canopy with three independent variables of $T_f$(foliage temperature), $T_g$(ground temperature) and $q_g$(ground specific humidity). The model was verified by comparative study with OSUID(Oregon State University One Dimensional Model) proved in HYPEX-MOBHLY experiment. As the result, both vegetation and soil characteristics can be emphasized as an important factor iii the analysis of heat flux in the boundary layer. From the numerical experiments, following heat flux characteristics are clearly founded simulation. The larger shielding factor(vegetation) increase of $T_f$ while decrease $T_g$. because vegetation cut solar radiation to ground. Vegetation, the increase of roughness and resistance, increase of sensible heat flux in foliage while decrease the latent heat flux in the foliage.

• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2006년도 추계학술대회
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• pp.336-339
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• 2006

With the steady depletion off fossil fuel reserves, hydrogen based energy sources become increasingly attractive. Therefore hydrogen production or separation technologies, such as Bas separation membrane based on adsorption technology, have received enormous attention in the industrial and academic fields. In this study, the transport mechanisms of the MTES (methyltriethoxysilane) templating silica/a-alumina composite membrane were evaluated by using unary, binary and quaternary hydrogen gas mixtures permeation experiments at unsteady- and steady-states. Since the permeation flux in the MTES membrane, through the experimental and theoretical study, was affected by molecular sieving effects as well as surface diffusion properties, the kinetic and equilibrium separation should be considered simultaneously in the membrane according to molecular properties. In order to depict the transient multi-component permeation on the templating silica membrane, the GMS (generalized Maxwell-Stefan) and DGM (dust Bas model) were adapted to unsteady-state material balance

• 한국지구과학회지
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• 제34권6호
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• pp.561-574
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• 2013

본 연구에서는 낙동강 강정고령보 근처에서 2011년 7월부터 2012년 9월까지 1년 이상 관측된 에너지 플럭스 자료의 분석을 통해 강 주변 농경지와 도시에 따른 플럭스 특징을 알아보고 향후 영향평가에 활용 가능한 자료인지 평가하고자 하였다. 연구 대상지는 농경지로 둘러싸인 시골지역과 도시공단 지역에 위치하였다. 현열 및 잠열 플럭스를 풍향에 따라 분석하였다. 여름에 바람이 강쪽에서 불어올 때 두 관측지점 모두 현열은 감소하고 잠열은 증가하는 형태를 보였다. 이는 강으로부터 전달된 수분에 의한 것으로 파악된다. 보웬비, 에너지 수지 닫힘, 운동량 플럭스, 안정도에 대한 분석 또한 이루어졌다. 두 지점간 보웬비를 비교한 결과 전 계절에 걸쳐 도시 지역의 보웬비가 농경지 지역의 보웬비보다 더 높았다. 에너지 수지 닫힘은 도시 지역에서 더 낮게 나타났는데 이는 도시 지역에서 저장항 계산이 배제되었기 때문으로 보인다. 운동량 플럭스는 여름과 겨울 두 계절 모두 도시 지역에서 더 높게 나타났다. 강한 난류를 보이는 주간과 여름에 불안정한 상태가 장시간 지속되었다. 이들 지점에서 관측된 자료는 향후 강이 주변지역에 미치는 영향에 대한 연구에 사용하기 적절한 것으로 보인다.

• 대한기계학회논문집A
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• 제35권1호
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• pp.33-37
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• 2011

디스플레이, 광학, 에너지 분야 부품의 미세형상화, 대면적화, 저가격화 요구에 대응하기 위하여 대면적 롤금형의 미세형상 가공기술개발에 대한 필요성이 대두되고 있다. 롤금형은 기존의 평판금형에 비해서 금형의 납기가 빠르고, 대면적화에 용이하며, 연속성형이 가능하다는 장점을 갖고 있다. 본 연구는 롤금형에 미세형상을 가공할 때 발생하는 형상오차의 원인을 규명하는 것을 목적으로 하고 있으며, 가공 현장에서 개선 가능한 요소로서 롤금형의 동적밸런싱 보정방안을 제시하고 있다. 기존보다 정밀한 동적밸런싱 보정을 통하여 롤금형의 질량불평형이 최대 90%까지 감소되었고, 롤금형의 진동량이 0.044 mm/sec (RMS)에서 0.004mm/sec (RMS)로 감소하였으며, 결과적으로 미세패턴의 형상정밀도가 개선되는 것을 확인할 수 있었다.

• 대한공간정보학회지
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• 제19권4호
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• pp.145-151
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• 2011

증발산(Evapotranspiration)은 생태학 수문학적으로 지표 특성을 표현하는 변수로서 지구 물 순환과 에너지 수지에 중요한 역할을 한다. 본 연구에서는 높은 지표거칠기를 고려하여 에너지 수지식을 기반으로 실제 증발산량을 산출하였다. 2009년 한반도를 대상으로 다양한 위성 자료와 관측 자료를 이용하여 연구를 수행하였다. 실제 증발산량 산출에 있어 중요한 변수인 현열은 다양한 입력 변수가 사용되어 계산 과정이 복잡하므로 본 연구에서는 경험적 계수인 B를 사용하여 현열 산출을 단순화하였다. 또한 본 연구에서는 현열 산출 시 중요한 변수인 공기역학적 저항을 고려하여 높은 지표거칠기를 반영한 실제 증발산량 모델을 제시하였다. 산출된 실제 증발산량은 Priestley-Taylor 가능 증발산량을 통한 검증(RMSE 1.0179mm/day, BIAS 0.4516mm/day)을 수행하였으며 높은 지표거칠기를 고려한 실제 증발산량이전반적으로 잘 산출되었음을 알 수 있었다.