• Transactions of the Korean Society of Mechanical Engineers B
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• v.35 no.6
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• pp.561-567
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• 2011

The inverse radiation analysis of a two-dimensional irregular configuration using unstructured triangular meshes is presented. In this study, an enclosure filled with an absorbing, emitting and scattering medium with diffusely emitting and reflecting opaque boundaries is considered. The finite volume method is applied to solve the radiative transfer equation in order to simulate the measured incident radiation values which are used as input data for the inverse analysis. The conjugate gradient method is adopted for the estimation of wall emissivities by minimizing the objective function at each iteration step. To verify the performance of the unstructured grid system, we compare the results with those using a structured grid system for the two-dimensional lopsided shape. The effect of measurement errors on the estimation accuracy is also investigated.

• Journal of the Korean earth science society
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• v.29 no.2
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• pp.128-139
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• 2008

Intercomparison among the three radiative transfer models (RTMs) which have been used in the studies for COMS, was carried out on the condition of aerosol-laden atmospheres. Also the role of aerosols in the atmospheric radiation budget was analyzed. The results (hereafter referred to as H15) from Halthore et al.'s study (2005) were used as a benchmark to examine the models. Aerosol Radiative Forcing (ARF) values from the three RTMs, calculated under two conditions of Aerosol Optical Thickness (AOT=0.08, 0.24), were systematically underestimated in comparison to H15 in the following shortwave components; 1) direct and diffuse irradiance at the surface, 2) diffuse upward fluxes at the surface and the top of the atmosphere, and 3) atmospheric absorbance. The ARF values for the direct and diffuse fluxes at the surface was $-10{\sim}-40Wm^{-2}$. The diffuse upward values became larger with increasing both AOT and Solar Zenith Angle (SZA). Diffuse upward/downward fluxes at the surface were more sensitive to the SZA than to the atmospheric type. The diffuse downward values increased with increasing AOT and decreasing SZA. The larger AOT led to surface cooling by exceeding the reduction of direct irradiance over the enhancement of diffuse one at the surface. The extinction of direct solar irradiance was due mainly to water vapor in tropical atmospheres, and to both ozone and water vapor in subarctic atmospheres. The effect of water vapor in the tropics was $3{\sim}4$ times larger than that of the ozone. The absorbance values from the three RTMs agree with those from H15 within ${\pm}10%$.

• Transactions of the Korean Society of Mechanical Engineers B
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• v.20 no.10
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• pp.3371-3380
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• 1996

Low resolution spectral modeling of water vapor is carried out by applying the weighted-sum-of-gray-gases model (WSGGM) to a narrow band. For a given narrow band, focus is placed on proper modeling of gray gas absorption coefficients vs. temeprature relation used for any solution methods for the Radiative Transfer Equation(RTE). Comparison between the modeled emissivity and the "true" emissivity obtained from a high temperatue statistical narrow band parameters is made ofr the total spectrum as well as for a few typical narrow bands. Application of the model to nonuniform gas layers is also made. Low resolution spectral intensities at the boundary are obtained for uniform, parabolic and boundary layer type temeprature profiles using the obtained for uniform, parabolic and boundary layer type temperature profiles using the obtained WSGGM's with 9 gray gases. The results are compared with the narrow band spectral intensities as obtained by a narrow band model-based code with the Curtis-Godson approximation. Good agreement is found between them. Local heat source strength and total wall heat flux are also compared for the cases of Kim et al, which again gives promising agreement.

• Transactions of the Korean Society of Mechanical Engineers B
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• v.28 no.5
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• pp.580-586
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• 2004

The ray effects of finite volume method (FVM) or discrete ordinate method (DOM) are known to show a non-physical oscillation in solution of radiative heat transfer on a boundary. This wiggling behavior is caused by the finite discretization of the continuous control angle. This article proposes a combined procedure of the Monte-Carlo and finite-volume method (CMCFVM) for solving radiative heat transfer in absorbing, emitting, and an-isotropically scattering medium with an isolated boundary heat source. To tackle the problem, which is especially pronounced in a medium with an isolated heat source, the CMCFVM is suggested here and successfully applied to a two-dimensional circular geometry.

• Korean Journal of Remote Sensing
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• v.13 no.2
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• pp.99-120
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• 1997

Solar radiation is scattered and absorbed atmospheric compositions in the atmosphere before it reaches the surface and, then after reflected at the surface, until it reaches the satellite sensor. Therefore, consideration of the radiative transfer through the atmosphere is essential for the quantitave analysis of the satellite sensed data, specially at shortwave region. This study examined a feasibility of using radiative transfer code for estimating the atmospheric effects on satellite remote sensing data. To do this, the flux simulated by LOWTRAN7 is compared with CAGEX data in shortwave region. The CAGEX (CERES/ARM/GEWEX Experiment) data provides a dataset of (1) atmospheric soundings, aerosol optical depth and albedo, (2) ARM(Aerosol Radiation Measurement) radiation flux measured by pyrgeometers, pyrheliometer and shadow pyranometer and (3) broadband shortwave flux simulated by Fu-Liou's radiative transfer code. To simulate aerosol effect using the radiative transfer model, the aerosol optical characteristics were extracted from observed aerosol column optical depth, Spinhirne's experimental vertical distribution of scattering coefficient and D'Almeida's statistical atmospheric aerosols radiative characteristics. Simulation of LOWTRAN7 are performed on 31 sample of completely clear days. LOWTRAN's result and CAGEX data are compared on upward, downward direct, downward diffuse solar flux at the surface and upward solar flux at the top of the atmosphere(TOA). The standard errors in LOWTRAN7 simulation of the above components are within 5% except for the downward diffuse solar flux at the surface(6.9%). The results show that a large part of error in LOWTRAN7 flux simulation appeared in the diffuse component due to scattering mainly by atmispheric aerosol. For improving the accuracy of radiative transfer simulation by model, there is a need to provide better information about the radiative charateristrics of atmospheric aerosols.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2002.11a
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• pp.360-361
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• 2002

대기 중의 에어로졸은 지구의 복사평형에 직·간접적으로 영향을 끼친다. 직접적인 영향으로는 에어로졸이 가시광선과 자외선 영역의 에너지를 산란 또는 흡수함으로써 기후에 영향을 미치며, 간접적으로는 microphysical process에 의한 구름의 특성을 변화시키거나 불균일적인 화학반응을 통해서 복사특성을 지니는 가스들을 변화시킴으로써 기후에 영향을 미친다. 또한 동북아 지역 및 인접한 태평양 지역은 중국과 인접해 있는 관계로 매년 봄철이민 고비사막이나 중국의 황토고원에서 발생한 황사(Asian Dust) 현상에 의해 많은 고통을 겪고 있다. (중략)

• Korean Chemical Engineering Research
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• v.50 no.6
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• pp.1049-1055
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• 2012

The fiber mat catalytic burner that uses infrared radiative heat obtained by flameless catalytic combustion was manufactured and tested to investigate its combustion characteristics. About 9 to 17% of combustion heat was released by sensible heat during the premixed catalytic combustion depend on combustion condition. To find out radiation intensity with distance between catalytic burner and sample, the equation that calculate the receiving surface of radiative energy under the fiber mat catalytic burner was driven. This equation was well correlated with the drying rate of melamine. The drying experiments were carried out to the melamine, wood chip and agricultural pallet by using the fiber mat catalytic burner and the energy efficiency was calculated from drying rate of them. The energy efficiency of the fiber mat catalytic burner reaches to 79% in maximum for drying of the wood chip.

• Proceedings of the Korea Multimedia Society Conference
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• 2001.11a
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• pp.56-59
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• 2001

OFDM 시스템은 부반송파의 직교성을 이용하는 특징으로 인하여 신호치 시간동기 및 주파수동기가 맞지 않은 경우 수신신호를 정확히 복조하기가 거의 불가능하다. 보호구간(Guard Interval)은 신호의 데이터 구간 일부분을 복사하여 심볼의 앞에 추가하는 CP(Cyolic Prefix)방식을 사용하고 있으며, 채널에서 발생하는 ISI(InterSymbol Interference)를 흡수하는 중요한 역할을 한다. 본 논문에서는 시간동기에 사용되어지는 보호구간을 여러 부구간으로 나눈 후, 이를 이용하여 심볼 타이밍 동기를 추정하고자 한다. 제안된 방법은 기존의 방법에 비해 성능의 손실없이 많은 계산량을 줄이는 방법으로서 수신기의 구조를 단순화시킬 수 있다. 여러 채널 환경에서의 모의 실험을 통해 제안한 방법과 기존의 방법을 비교하였다.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 1999.10a
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• pp.319-322
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• 1999

최근 전지구적인 규모로 일어나고 있는 기상이변과 엘리뇨(El Nino)와 같은 현상들은 대기중 탄산가스농도의 증가와 그로 인한 지구온난화가 주요 원인중의 하나로 추정되고 있다. 이산화탄소를 위시한 여러 온난화가스들은 지표면에서 방출되는 태양의 복사열을 흡수하여 대기권 밖으로 열의 이동을 차단하는 효과를 발휘한다. 이러한 온난화 현상은 화석연료의 사용으로 대표되는 인간의 산업활동과 밀접한 연관성을 띠는 것으로 밝혀졌다 (김＆이, 1999).(중략)

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2002.04a
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• pp.77-78
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• 2002

동북아 지역은 급속한 산업 및 경제활동 증가로 세계의 주요 오염 지역으로 대두되고 있다. 대기오염 물질의 Global 이동확산은 어느 특정지역에서 다른 지역으로 광범위하게 이동 확산하기 때문에 이에 따른 오염과 피해 사이에 시간과 공간적인 차이가 존재하고 있으며, 그 인과관계도 불명확한 상황이다. 한편, 사막에서 발생한 모래먼지는 시정을 악화시키며 이들 중 미세한 입자(0.1-10$\mu\textrm{m}$)는 산란과 흡수를 통하여 대기의 복사평형과 기후변화에 커다란 영향을 미칠 수 있다(Carlson, 1980; Duce, 1980). (중략)