• Proceedings of the Korea Air Pollution Research Association Conference
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• 2001.11a
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• pp.283-284
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• 2001

라이다를 이용한 지구환경 감시 기술이 발전하고 대기 중 에어러솔에 대한 전지구적인 관측자료의 필요성이 증가하고 있다. 이와 동시에 관측결과의 신뢰성을 높이는데 필수적인 에어러솔에 대한 기본 정보, 특히 S-ratio(extinction to backscattering ratio)에 대한 데이터 베이스가 요구되고 있다. 특히, 2004년 발사 예정인 위성탑재 라이다 ESSP3(Earth System Science Pathfinder 3)와 같이 전 지구를 관측대상으로 하는 경우에는 전지구적인 S-ratio 자료가 특별히 요구된다. (중략)

• Journal of the Korean Association of Geographic Information Studies
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• v.15 no.1
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• pp.184-196
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• 2012

Biomass burning activities(BBA) are caused by both natural and anthropogenic origins. Due to emissions of greenhouse gases and atmospheric aerosols during the burning process, BBA has been known to be one of important sources of atmospheric pollution and the climate change. However, the monitoring of BBA and its effects on atmospheric environment are not simple. This study evaluates the trends of BBA and its impact on atmospheric environment by using earth observing satellite. The results show that the most BBA were found over ever green, green vegetation types, and irrigated land cover types in study region. The trends of BBA and aerosol optical thickness which represents relative aerosol loading in the atmosphere, show similar pattern. Aerosol increases caused by BBA highlight the effectiveness of these mechanisms and would affect the regional atmospheric environment and climate change.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2005.11a
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• pp.315-316
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• 2005

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2010.04a
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• pp.303-305
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• 2010

• Proceedings of the Korea Air Pollution Research Association Conference
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• 1999.04a
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• pp.239-240
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• 1999

• Atmosphere
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• v.21 no.1
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• pp.57-67
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• 2011

Aerosol lidar ratio (extinction-to-backscatter ratio) at 532 nm was determined using 4-year measurements of elastic-backscatter lidar and sky radiometer at Seoul National University of Seoul, Korea. The mean lidar ratio (with standard deviation) based on 4 years of measurements is found to be $61.7{\pm}16.5$ sr, and weak seasonal variations are noted with a maximum in JJA ($68.1{\pm}16.8$ sr) and a minimum in DJF ($57.2{\pm}17.9$ sr). The lidar ratios for clean, dust, and polluted conditions are estimated to be $45.0{\pm}9.5$ sr, $51.7{\pm}13.7$ sr, and $62.2{\pm}13.2$ sr, respectively. While the lidar ratio for the polluted condition is appears to be consistent with previous studies, clean and dust conditions tend to have larger ratios, compared to previous estimates. This discrepancy is thought to be mainly due to the anthropogenic aerosols existing throughout the year around Seoul, which may cause increased lidar ratios even for clean and dust conditions.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2008.04a
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• pp.77-78
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• 2008

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2006.04a
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• pp.331-333
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• 2006

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2006.04a
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• pp.226-227
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• 2006

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2008.10a
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• pp.496-497
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• 2008