• Proceedings of the Korea Air Pollution Research Association Conference
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• 2008.10a
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• pp.118-119
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• 2008

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2008.10a
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• pp.260-261
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• 2008

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2010.04a
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• pp.557-558
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• 2010

• Journal of the Korean earth science society
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• v.34 no.7
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• pp.693-710
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• 2013

This study investigates the distribution of suspended particulates during the Asian dust period in Busan, Korea in the spring of 2009. Weather map and automatic weather system (AWS) data were used to analyze the synoptic weather conditions during the period. Particulate matter 10, laser particle counter data, satellite images and a backward trajectories model were used to analyze the aerosol particles distribution and their origins. In Case 1 (20 February 2009), when the $PM_{10}$ concentration increased, the aerosol volume distribution of small ($0.3-1.0{\mu}m$) particles decreased, while the concentration of large ($1.0-10.0{\mu}m$) particles increased. When the $PM_{10}$ concentration decreased, the aerosol volume distribution was observed to decrease as well. The prevailing winds changed from weak northerly winds to strong southwesterly winds when the concentration of the large particles increased. The correlation coefficient between the $PM_{10}$ concentration and aerosol volume distribution of large particles showed a high positive value of over 0.9. The results from the trajectory model show that the Asian dust originated in the Gobi desert and the Nei Mongol plateau. In Case 2 (25 April 2009), when the $PM_{10}$ concentration increased, the aerosol volume concentration of small ($0.3-0.5{\mu}m$) particles decreased, but the concentration of large ($0.5-10.0{\mu}m$) particles increased. The opposite was observed when the $PM_{10}$ concentration decreased. The prevailing winds changed from northeasterly winds to southwesterly and northeasterly winds. The correlation coefficient between the $PM_{10}$ concentration and aerosol volume distribution of large particles ($1.0-10.0{\mu}m$) showed a high positive value of about 0.9. The results from the trajectory model show that the Asian dust originated in Manchuria and the eastern coast of China.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2002.11a
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• pp.334-336
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• 2002

최근 이십여년 동안 대기 중에 존재하는 저분자량 카르복실산의 역할에 대한 관심이 증가되어 왔다. 주로 아세트산과 포름산으로 존재하는 저분자량의 카르복실산은 대류권의 여기저기에 기체상으로 존재하거나, 수용액 상이나 혹은 에어로솔이나 입자상물질의 표면에 녹거나 흡착되어 있는 형태로 존재한다. (중략)

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2008.10a
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• pp.147-148
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• 2008

• The Science & Technology
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• v.33 no.10 s.377
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• pp.78-79
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• 2000

나노입자의 제조 및 성장제어와 열 및 물질전달과 에어로솔 공학분야의 연구에 주력하고 있는 최만수 교수(44세). 최근에는 나노입자의 융합속도를 제어하는 새로운 나노입자 성장제어 기술을 개발해 학계의 관심을 모으고 있다. 최교수는 앞으로 융합촉진을 이용하는 나노입자 제어기술을 복합나노입자를 포함한 여러 다양한 나노입자의 제조와 나노물질의 제조에 응용해 나갈 것이며 이론적 모델리의 개발도 병행해 나갈 계획이다.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2002.11a
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• pp.326-327
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• 2002

제주도 고산은 지역자체내의 대기오염물질이 거의 없는 우리나라의 대표적인 배경농도지역이며, 지리적 특성상 동북아시아에서 대기오염물질의 장거리이동 특성을 규명하는데 적합한 지역으로 알려져 있다. 고산에 대한 활발한 연구를 통해 장기간 TSP 측정자료가 모아졌으나, 아직까지 그 해석에 대한 통계적인 분석과 이동특성에 관한 해석을 위한 역궤적 분석은 미흡하다. 이에 본 발표에서는 1992년 3월부터 2002년 2월까지 고산에서 측정한 입자상 무기이온 성분의 농도를 장기간의 역궤적 분석결과와 함께 통계적인 방법으로 해석하고자 하였다. (중략)

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2008.04a
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• pp.571-572
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• 2008

• Korean Journal of Remote Sensing
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• v.34 no.3
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• pp.507-517
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• 2018

Aerosol optical depth (AOD) data retrieved by the Communication, Ocean and Meteorological Satellite (COMS) during 2011-2014 were compared with AOD measurements from 134 Aerosol Robotic Network (AERONET) sites over the East Asia. Overall, COMS and AERONET AODs were weakly correlated (R = 0.297). The agreement between COMS and AERONET AODs was improved when data from near Korean peninsula sites were selected (R = 0.475). Regression analysis results for each AERONET site are vary from R=0.026 at AOE_Baotou to 0.905 at DRAGON_Anmyeon. It was also shown that the bias in COMS AOD was not systematic with respect to effective radius, precipitable water, surface reflectance, and sun zenith angle. Together, these results suggest that COMS AOD measurements may be suitable for near Korea. Finally, the current results will help to improve the retrieval algorithm and vary when using alternative COMS AOD version in the future.