• 대기
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• 제21권2호
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• pp.131-142
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• 2011

Spectral solar irradiances were observed using a visible and UV Multi-Filter Rotating Shadowband Radiometer on the rooftop of the Science Building at Yonsei University, Seoul ($37.57^{\circ}N$, $126.98^{\circ}E$, 86 m) during one year period in 2006. 1-min measurements of global(total) and diffuse solar irradiances over the solar zenith angle (SZA) ranges from $20^{\circ}$ to $70^{\circ}$ were used to examine the effects of clouds and total optical depth (TOD) on enhancing four solar irradiance components (broadband 395-955 nm, UV channel 304.5 nm, visible channel 495.2 nm, and infrared channel 869.2 nm) together with the sky camera images for the assessment of cloud conditions at the time of each measurement. The obtained clear-sky irradiance measurements were used for empirical model of clear-sky irradiance with the cosine of the solar zenith angle (SZA) as an independent variable. These developed models produce continuous estimates of global and diffuse solar irradiances for clear sky. Then, the clear-sky irradiances are used to estimate the effects of clouds and TOD on the enhancement of surface solar irradiance as a difference between the measured and the estimated clear-sky values. It was found that the enhancements occur at TODs less than 1.0 (i.e. transmissivity greater than 37%) when solar disk was not obscured or obscured by optically thin clouds. Although the TOD is less than 1.0, the probability of the occurrence for the enhancements shows 50~65% depending on four different solar radiation components with the low UV irradiance. The cumulus types such as stratoculmus and altoculumus were found to produce localized enhancement of broadband global solar irradiance of up to 36.0% at TOD of 0.43 under overcast skies (cloud cover 90%) when direct solar beam was unobstructed through the broken clouds. However, those same type clouds were found to attenuate up to 80% of the incoming global solar irradiance at TOD of about 7.0. The maximum global UV enhancement was only 3.8% which is much lower than those of other three solar components because of the light scattering efficiency of cloud drops. It was shown that the most of the enhancements occurred under cloud cover from 40 to 90%. The broadband global enhancement greater than 20% occurred for SZAs ranging from 28 to $62^{\circ}$. The broadband diffuse irradiance has been increased up to 467.8% (TOD 0.34) by clouds. In the case of channel 869.0 nm, the maximum diffuse enhancement was 609.5%. Thus, it is required to measure irradiance for various cloud conditions in order to obtain climatological values, to trace the differences among cloud types, and to eventually estimate the influence on solar irradiance by cloud characteristics.

• Journal of Mechanical Science and Technology
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• 제16권10호
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• pp.1346-1354
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• 2002

The purpose of this work is to study the effects of specularly reflecting wall under the combined radiative and laminar free convective heat transfer in an infinite square duct. An absorbing and emitting gray medium is enclosed by the opaque and diffusely emitting walls. The walls may reflect diffusely or specularly. Boussinesq approximation is used for the buoyancy term. The radiative heat transfer is evaluated using the direct discrete ordinates method. The parameters under considerations are Rayleigh number, conduction to radiation parameter, optical thickness, wall emissivity and reflection mode. The differences caused by the reflection mode on the stream line, and temperature distribution and wall heat fluxes are studied. Some differences are observed for the categories mentioned above if the order of the conduction to radiation parameter is less than order of 10$\^$-3/ fer the range of Rayleigh number studied. The differences at the side wall heat flux distributions are observed as long as the medium is optically thin. As the top wall emissivity decreases, the differences between these two modes are increased. As the optical thickness decreases at the fixed wall emissivity, the differences also increase. The difference of the streamlines or the temperature contours is not as distinct as the side wall heat flux distributions. The specular reflection may alter the fluid motion.

• 대기
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• 제14권2호
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• pp.11-22
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• 2004

A technique on atmospheric correction algorithm to the multi-band reflectance of Landsat TM imagery has been developed using an atmospheric radiation transfer model for eliminating the atmospheric and surface diffusion effects. Despite the fact that the technique of satellite image processing has been continually developed, there is still a difference between the radiance value registered by satellite borne detector and the true value registered at the ground surface. Such difference is caused by atmospheric attenuations of radiance energy transfer process which is mostly associated with the presence of aerosol particles in atmospheric suspension and surface irradiance characteristics. The atmospheric reflectance depend on atmospheric optical depth and aerosol concentration, and closely related to geographical and environmental surface characteristics. Therefore, when the effects of surface diffuse and aerosol reflectance are eliminated from the satellite image, it is actually corrected from atmospheric optical conditions. The objective of this study is to develop an algorithm for making atmospheric correction in satellite image. The study is processed with the correction function which is developed for eliminating the effects of atmospheric path scattering and surface adjacent pixel spectral reflectance within an atmospheric radiation model. The diffused radiance of adjacent pixel in the image obtained from accounting the average reflectance in the $7{\times}7$ neighbourhood pixels and using the land cover classification. The atmospheric correction functions are provided by a radiation transfer model of LOWTRAN 7 based on the actual atmospheric soundings over the Korean atmospheric complexity. The model produce the upward radiances of satellite spectral image for a given surface reflectance and aerosol optical thickness.

• Radiation Oncology Journal
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• 제11권1호
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• pp.79-82
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• 1993

본 연구는 1989년 10월부터 1992년 3월까지 아산재단 서울중앙병원에서 원발성 중추신경계 림프종으로 진단 받은 10명의 환자를 대상으로 하였다. 병리적 진단을 위한 조직은 5명에서 개두술에 의한 종양절제술로 얻어졌으며 나머지는 정위적 조직생검에 의해 얻어졌다. 성별분포는 남녀가 각 5명이었고 연령분포는 28세부터 72세로 평균연령은 45세로 나타났다. Working Formulation에 의한 세포아형은 7명에서 diffuse large cell type이었고 3명은 diffuse mixed cell type이었다. 전산화 단층촬영 결과 6명은 단일병소로 나타났으며 4명은 다발성병소로 나타났다. 치료는 전 환자가 전뇌방사선 조사를 4000 cGy/20 fx을 받은 후 원발병소에 2000 cGy/10 fx을 조사하여 총 6000 cGy를 시행하였다. 척수액 검사상 양성인 6명은 전뇌조사와 척수강내 항암제 투여를 받았으며 그중 1명은 척수강내 항암제 투여 3회 실시후 척수방사선 조사를 받았다. 척수액 검사상 음성인 4명중 3명은 전뇌조사만 실시했고 나머지 1명은 방사선 조사전 전신 항암제 투여를 받았다. 추적관찰기간은 7개월에서 26개월이었으며 평균 추적기간은 8개월 이었다. 1년 생존율은 86%이었고 2년 생존율은 69%로 나타났다. 현재까지 2명이 척수강내 재발 후 뇌실질내 재발로 사망했으며, 반면 7명의 환자는 방사선 치료후 병소가 완전히 없어졌다. 위의 결과로 볼때 원발성 중추신경계 림프종의 방사선 치료에 대한 월등한 초기반응과 원격 전이 가 적은 것을 고려하여 원발병소에 분할치료 방법들을 통한 전체 조사량을 증가시키는 것이 효과적이라고 생각되며 척수액 검사상 양성인 경우는 척수 방사선 조사와 척수강내 항암제를 함께 쓰는 좀더 적극적 치료가 필요하리라 생각된다.

• 한국생물환경조절학회:학술대회논문집
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• 한국생물환경조절학회 1998년도 정기총회 및 학술논문 발표요지
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• pp.27-32
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• 1998

국내에 보급되어 있는 유리온실은 네덜란드에서 수입된 벤로형(Venlo type or Dutchlite)과 벤로형에 비해서 동고가 높으며 온실 한 동의 폭이 상대적으로 큰 광폭형(widespan type)이 대부분을 차지하고 있다. 벤로형 은실의 측고는 3.5~4.0m로서 다소 차이가 있으나, 한 동의 폭과 지붕경사면의 길이가 일정하기 때문에 온실의 지붕경사각은 대부분 22$^{\circ}$를 나타낸다. (중략)

• 대한기계학회논문집B
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• 제24권1호
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• pp.9-20
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• 2000

An analysis of heat and mass transfer has been carried out for multi-wafer Low Pressure Chemical Vapor Deposition (LPCVD). Surface radiation analysis considering specular radiation among wafers, heaters, quartz tube and side plates of the reactor has been done to determine temperature distributions of 150 wafers in two dimensions. Velocity, temperature and concentration fields of chemical gases flowing in a reactor with multi-wafers have been then determined, which determines Si deposition growth rate and uniformity on wafers using two different surface reaction models. The calculation results of temperatures and Si deposition have been compared and found to be in a reasonable agreement with the previous experiments.

• 태양에너지
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• 제9권3호
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• pp.3-12
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• 1989

Semi-greenhouse type solar-dehumidification drying of oak was carried out to investigate the possibility to dry wood using solar energy in Korea. The energy balance equation was set up, considering all the energy requirements, and the solar radiation was calculated to analyze the efficiencies of solar dryer with and without the dehumidifier. The average temperature inside dryer and collector rose up to $52^{\circ}C$ and $70^{\circ}C$, respectively. The average daily total beam, diffuse, and ground-reflected radiations were 7.27MJ, 8.70MJ, and 0.33MJ on the roof and 2.08MJ, 4.84MJ, and 5.37MJ on the south wall collector, respectively. Heat efficiency of solar dryer was 14.04% with dehumidifier and 13.13% without dehumidifier. The energy required to remove 1g of water from wood was 0.0289MJ/g in solar-dehumidification drying and 0.0310 MJ/g in semi-greenhouse type solar drying.

• 한국지구과학회지
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• 제29권2호
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• pp.128-139
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• 2008

본 연구에서는 에어러솔 대기 상태에서 국내 COMS 연구자들이 사용하는 세 개의 단파 복사전달모델에서 산출된 복사속 성분을 비교분석하였으며, 대기 복사 수지에서 에어러솔 역할도 분석하였다. 국내 모델들의 평가를 위하여, 15개 모델값을 평균한 Halthore et al.(2005) 결과를 기준값으로 사용하였다. 두 종류 에어러솔 농도(AOT=0.08, 0.24)에서 조사된 열대 또는 한대 대기의 에어러솔 강제력은 지표에서의 하향 일사 및 상향 산란, 대기 상부의 상향 산란, 그리고 대기 흡수도의 복사 성분들에 있어서 국외 연구에 비하여 국내 결과들에서 체계적으로 약하게 나타났다. 에어러솔 강제력은 지표에서의 하향 일사에 대하여 $-10{\sim}-40Wm^{-2}$ 이었으며, 지표 및 대기 상부의 상향 산란의 경우에 상대적으로 큰 태양천정각과 고농도 에어러솔 상태에서 컸다. 두 종류 에어러솔 조건에서 지표에서의 하향 및 상향 산란값들은 대기 종류보다는 태양천정각에 더 민감하였다. 하향 산란은 상대적으로 작은 태양천정각과 고농도 에어러솔 조건에서 컸다. 에어러솔 농도 증가는 하향 산란 증가에도 불구하고 하향 직달 일사의 감소가 이를 초과함으로써 지표 냉각을 유도하는 것으로 조사되었다. 동일한 에어러솔 농도 및 태양천정각 조건에서 직달일사 소산은 열대 대기에서는 주로 수증기, 그리고 한대 대기에서는 수증기뿐만 아니라 오존에도 기인하는 것으로 조사되었다. 특히 열대 대기에서는 수증기의 역할이 오존에 비하여 $3{\sim}4$배 컸다. 저농도 및 고농도 에어러솔 대기에서 대기 흡수도는 국내외 연구간에 ${\pm}10%$ 내에서 일치하였다.

• 한국환경복원기술학회지
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• 제16권4호
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• pp.27-40
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• 2013

These day morden cities have serious climatic problems due to enviornmental load caused by excessive development of urbanization. As technological improvement to answer to various ecological disasters and climate changes are also called on the field of construction, inter-disciplinary studies linked to the estabilishment of sustainable energy generation systems and enviornmental control is needed in a consilient point of view. This study aims to analyse optimal site conditions for photovoltaic system and green roof planting through solar radiation simulation in a integrated perspective. In so doing, it seeks to proffer basic study for developing a sound use of roof area that is sustainable in environmental and resources aspects. A computer simulation showed that, in the case of total seasonal solar radiation, summer season resulted 312.5kWh in 35% of total annual solar radiation. This season indicated the lowest radiation rate of the year for direct sunlight in 45.8% of total seasonal solar radiation. Due to such solar radiation simulation, at the largest optimal planting area, Glechoma hederacea var. longituba secured $719.16m^2$ of gross roof area.

• 한국태양에너지학회 논문집
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• 제35권1호
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• pp.9-19
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• 2015

Pyranometer have many uncertainty factors (sensitivity function, thermal offset, other spectral effect, geometric, environment, and equipment etc.) than pyrheliometer. The solution for most of the uncertainty factors have been researched, but the problem for thermal offset is being continued research so far. Under the clear sky, due to the thermal offset of pyranometer, the diffuse and global radiation have been negative value for the nighttime and lower value for the daytime, respectively. In order to understand the uncertainty of the thermal offset effect, solar radiation are observed and analyzed using Ji and Tsay method and data from modified pyranometer. As a result of performing temperature correction using the modified pyranometer, the slope (dome factor; k) and intercept ($r_0$) from a linear regression method are 0.064 and $3.457g{\cdot}m^{-2}{\cdot}k^{-1}$, respectively. And the solar radiation is decreased significantly due to the effect of thermal offset during nighttime. The solar radiation from modified pyranometer increased approximately 8% higher than its observed by general pyranometer during daytime. By the way, these results did not generalize because its result is for only single case in clear sky. Accordingly, it is to required for accurate results obtained by the various cases (clear, cloudy and rainy) with longterm observations.