• 대한원격탐사학회지
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• 제32권5호
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• pp.435-452
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• 2016

천리안(Communication, Ocean, and Meteorological Satellite) 위성자료로부터 Cho et al.(2015)에 의해 개발된 분리대기창법(split-window method: CSW_v2.0)을 적용하여 현업적으로 지표면온도를 산출하고 있다. CSW_v2.0으로부터 산출된 지표면온도는 MODIS 지표면온도와 비교하였을 때 적절한 수준의 정확도로 산출되었으나 역전층이나 기온감률이 클 때 상대적으로 오차가 크게 발생하였다. 이를 해결하기 위해 지표 경계층에서의 기온의 일변동을 복사전달모델에 처방하여 모의자료를 구축한 후 이를 이용하여 지표면온도 산출 알고리즘을 개선하였다(CSW_v3.0). CSW_v3.0에서는 복사전달모델에 처방된 지표면온도와 복사전달모델로부터 산출된 지표면온도간의 상관계수가 기존 알고리즘과 동일한 수준인 0.99 이상을 유지하면서 편의는 -0.03 K에서 -0.012 K, RMSE는 1.39 K에서 1.138 K로 감소하였다. CSW_v2.0에서 역전층이나 기온감률이 클 때, 휘도온도차와 방출율 차가 클 때 발생하는 계통적 오차를 개선된 알고리즘에서는 편의와 RMSE를 10-30% 감소시켜 상당 부분 개선하였다. CSW_v3.0으로부터 산출된 지표면온도와 MODIS 지표면온도와의 간접 검증에서는 상관계수가 0.986에서 0.985로 높은 상관성을 유지하면서 편의는 0.629 K에서 -0.049 K, RMSE는 2.537 K에서 2.502 K로 오차를 감소시켰다.

• 대한원격탐사학회지
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• 제30권5호
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• pp.627-639
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• 2014

인공위성의 가시 영역 관측으로부터 에어로솔의 정량적인 정보를 산출하는데 있어, 지표면 반사도의 보정은 매우 중요한 역할을 한다. 이에 본 연구에서는 두 가지 방법을 이용하여 천리안위성의 기상탑재체로부터 관측된 가시채널의 반사도로부터 지표면 반사도를 산출하고, 상호 비교 하여 정확도를 검증하고자 하였다. 첫 번째 방법은 최소 반사도법으로, 동일한 화소에서 일정 기간 동안 관측된 반사도 중 최소값이 에어로솔에 의한 영향 없이 지표반사에 의한 영향만을 포함한다는 가정을 기반으로, 대기산란 효과를 보정하여 지표면 반사도를 산출하는 방법이다. 두 번째 방법은 미리 알고 있는 에어로솔 정보를 고려하여 대기-에어로솔 효과를 보정함으로써 지표면 반사도를 얻는 것으로 본 연구에서 대기 보정법 이라 칭한다. 두 번째 방법을 적용하기 위해서는 정확한 에어로솔 정보가 요구되므로, 에어로솔 광학두께의 오차범위가 0.01 (${\geq}440nm$) 이내인 것으로 알려진 AERONET의 산출물을 이용하였다. 본 연구의 주요 목적은 최소 반사도법을 통하여 산출되는 지표면 반사도가 어느 정도의 정확도를 가지는지를 파악하는데 있어, 대기 보정법을 통하여 산출되는 값을 기준 값으로 두고 비교 분석을 수행하였다. 또한, 대기 중 존재하는 배경광학두께가 최소 반사도법의 정확도에 미치는 영향을 분석해보고자 하였다. 서울 지역에서 2012년 봄철 기간(3월 ~ 5월)동안 AERONET 관측지점에서 산출된 결과를 분석 한 결과, 대기 보정법을 통해 산출된 지표면 반사도의 평균이 0.108로 나타났고, 배경광학두께에 대한 고려 없이 최소 반사도법을 통하여 산출된 지표면 반사도는 그에 비해 약 0.012 높은 값을 보였다. 한 편 배경광학두께를 고려하였을 경우 그 차이는 0.010으로 감소하여, 정확도 향상에 기여하였음을 확인하였다.

• 한국대기환경학회지
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• 제2권1호
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• pp.55-72
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• 1986

This study was made to determine the factors involving personal exposure levels of nitrogen dioxide for housewives living in urban area in two seasons, winter and summer. Nitrogen dioxide was measured with a small passive sampler containing triethanolamine. The samplers were set for 24 hours at three points. They were places: on the collar of the housewife to investigate the personal exposure level, near the TV in the living room (indoor level), and near the porch of their house (outdoor level). The subjects recorded the times of cooking using a gas range, using a kitchen ventilator, passive smoking, kerosene heater, total number of minutes at an open window, going out of home, etc.$\ldots. There was an apparent increase in personal exposure level in the case of the unvented heater and also an increase by cooking on a gas range. There was no marked increase in the other situations. There was an increase in the indoor level by cooking on a gas range, only in western style cooking in the winter season. Through these observations, we concluded that personal exposure level of nitrogen dioxide was strongly related to indoor nitrogen dioxide level, and factors involving indoor nitrogen dioxide level seemed different between winter and summer. The most significant difference in nitrogen dioxide level was indoor pollution in the winter and the outdoor environment in the summer. The maximum personal exposure level appeared in the western and tenement house in the winter and the traditional korean house in the summer.

• 한국대기환경학회지
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• 제16권4호
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• pp.381-388
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• 2000

Ceramic foam prepared with cordierite as a starting material by foam method was tested to evaluate the feasibility as a filter for the dust collection in hot gas. Two different types of agents Benzethonium chloride (BZTC, C27H42NO2Cl) and Sodium Lauryl Sulfate(SLS, CH3(CH2)11OSO3Na) were used as foaming agents in foaming process. Porosityof ceramic foam was about 80% and mean pore size were 100${\mu}{\textrm}{m}$ for SLS agent and 200 ${\mu}{\textrm}{m}$ for BZTC. It was observed that ceramic foam was composed of continuous macro-pore structure with opening windows interconnecting macro-pores. The surface of ceramic foam support of was coated with cordierite particles ranged from 20${\mu}{\textrm}{m}$ to 50${\mu}{\textrm}{m}$ Meso-pore size in the coating layer on ceramic foam was below 10${\mu}{\textrm}{m}$. While air permeability of the support increased with increasing macro-pore size coated ceramic filters showed a constant permeability without regard to the macro-pore size of the support. The permeabuilities of support varied in the range of 600$\times$10-13m2 to 1000$\times$10-13m2. For the case of coated ceramic filter it was about 200$\times$10-13m2. As a result of particle trapping test by using fly ash the particle removal efficiency was over the 99.9%.

• 한국군사과학기술학회지
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• 제17권1호
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• pp.8-14
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• 2014

Brightness temperature spectra acquired from FTIR(Fourier Transform Infrared)-SCADS (Standoff Chemical Agent Detection System) could be available for detection and identification of the chemical agents and pollutants from different background. IR spectrum range of 770 to 1350 $cm^{-1}$ is corresponding to "atmospheric window". A 2-dimensional(2D) brightness temperature spectrum was drawn from combining each data point through automatic continuous scanning of FTIR along with altitude and azimuth. At higher altitude, temperature of background was decreased but scattering effect of atmospheric gases was increased. Increase in temperature difference between background and blackbody in SCADS at higher temperature causes to increases in peak intensity of $SF_6$. This approach shows us a possibility that 2D visual information is acquired from scanning data with a single FTIR-SCADS.

• 대기
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• 제12권4호
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• pp.69-90
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• 2002

The infrared and microwave satellite observations have been used to derive the information of hydrometeors (i.e., cloud and precipitation) and atmospheric temperature. The observations were made by the Nimbus-4 Infrared Interferometer Spectrometer (IRIS) in 1970, and by the Microwave Sounding Unit (MSU) during the period 1980-99, which had channel 1~4 (Chl~4). The IRIS, which has a field of view of ~100 km, has been utilized to examine the cirrus and marine stratus clouds. The cirrus and stratus distributions were obtained, respectively, based on the spectral difference in the infrared window region, and the absorption of water vapor and $CO_2$ in the spectral region $870-980cm^{-1}$. The MSU Ch1 data has been used for low tropospheric temperature and hydrometeors, while the Ch2, Ch3 and Ch4, respectively, for the thermal state of midtroposphere, tropopause, and lower stratosphere. The climatic aspects of El Ni$\tilde{n}$o, Quasi-Biennial Oscillation (QBO) and temperature trends over the globe are discussed with the MSU data. This study suggests that the IRIS and MSU data are useful for monitoring the hydrometeors and atmospheric thermal state in climate system.

• 대기
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• 제25권4호
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• pp.577-589
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• 2015

An unusual long-period and heavy snowfall occurred in the Yeongdong region from 6 to 14 February 2014. This event produced snowfall total of 194.8 cm and the recordbreaking 9-day snowfall duration in the 103-year local record at Gangneung. In this study, satellite-derived cloud-top brightness temperatures from the infrared channel in the atmospheric window ($10{\mu}m{\sim}11{\mu}m$) are examined to find out the characteristics of clouds related with this heavy snowfall event. The analysis results reveal that a majority of precipitation is related with the low-level stratiform clouds whose cloud-top brightness temperatures are distributed from -15 to $-20^{\circ}C$ and their standard deviations over the analysis domain (${\sim}1,000km^2$, 37 satellite pixels) are less than $2^{\circ}C$. It is also found that in the above temperature range precipitation intensity tends to increase with colder temperature. When the temperatures are warmer than $-15^{\circ}C$, there is no precipitation or light precipitation. Furthermore this relation is confirmed from the examination of some other heavy snowfall events and light precipitation events which are related with the low-level stratiform clouds. This precipitation-brightness temperature relation may be explained by the combined effect of ice crystal growth processes: the maximum in dendritic ice-crystal growth occurs at about $-15^{\circ}C$ and the activation of ice nuclei begins below temperatures from approximately -7 to $-16^{\circ}C$, depending on the composition of the ice nuclei.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 1999년도 Proceedings of International Symposium on Remote Sensing
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• pp.135-139
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• 1999

Wind velocity is one of the primary variables for describing atmospheric state from GMS-5. And its accurate depiction is essential for operational weather forecasting and for initialization of NWP(Numerical Weather Prediction) models. The aim of this research is to incorporate imagery from other available spectral channels and examine the error characteristics of winds derived from these images. Multi spectral imagery from GMS-5 was used for this purpose and applied to Korean region with together BoM(Bureau of Meteorology). The derivation of wind velocity estimates from low and high resolution visible, split window infrared, and water vapor images, resulted in improvements in the amount and quality of wind data available for forecasting.

• 한국실내디자인학회논문집
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• 제24권4호
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• pp.91-98
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• 2015

Double skin façade is known that several features affected the building energy and daylighting performance. That is why the envelope is able to consist of all architectural materials such as glass, aluminum, wood and insulation for vision of residents and workers in buildings. Its specifications is very diverse according to the building designers and building owners. In recent times, visual environment became a major focus and resulted in the development of cutting edge engineering of diverse glazing systems and shading devices by growing interests of friendly environment. Thus this research has evaluated the fluctuations of interior lighting and atmospheric conditions based on double skin facade systems. Especially in terms of daylighting environment as dependent on solar variations, this research provides quantitative analysis of interior lighting conditions and how it affects the living conditions as well as improve the design of interior spaces.

• 한국대기환경학회:학술대회논문집
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• 한국대기환경학회 2001년도 추계학술대회 논문집
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• pp.307-308
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• 2001

본 연구는 서울, 청주, 춘천 세 개 도시 대기에서의 입자상 물질에 대한 분석을 Electron Probe X-ray Microanalysis(EPMA)를 이용한 단일 입자 분석법으로 행하였다. 단일 입자 분석법은 개개 입자의 형상과 크기 그리고 화학 조성에 대한 정보를 동시에 제공하기 때문에 개개 입자의 생성, 이동, 반응 그리고 환경에의 영향에 대한 자세한 정보를 얻을 수 있다. 또한 최근에 개발된 ultrathin window를 장착한 EPMA 분석법(Low-Z EPMA)은 종래의 통상적인 EPMA 방법으로는 분석하기 어려웠던 탄소, 질소, 산소 등의 원소를 정량적으로 분석할 수 있다. 따라서 도시 대기의 중요 구성 입자상 물질인 황산염, 질산염, 암모늄염, 유기 입자 등도 포함하여 도시 대기 입자 분석에 유용하게 활용된다. (중략)