東南亞生質燃燒源區及下風區氣膠與雲凝結核特性探討:泰北安康山與台灣鹿林山之比較分析

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東南亞生質燃燒源區及下風區氣膠與雲凝結核特性探討:泰北安康山與台灣鹿林山之比較分析

葉宗鑫 , Masters　　Advisor：林能暉;蕭大智　　

繁體中文

生質燃燒；雲凝結核；鹿林山； biomass burning ； cloud condensation nuclei ； CCN

Abstract │ Reference (110) │ Times Cited (1) │ Altmetrics

Abstract 〈TOP〉

Parallel Abstract 〈TOP〉

Indochina artificial activities cause a lot of biomass burning events in each spring (dry) season. The interaction between cloud and aerosol will not only affect radiation budget and water circulation system, but also the climate change and human health. According to above, the interaction must be taken into an issue, but the seldom research in the past literatures. In this study, we will investigate the artificial activities in Indochina, and discuss its interaction and influence.

Because atmospheric aerosols chemical composition, mixed patterns, and particle size can affect the formation of the cloud condensation nuclei, so we used CCN counter, SMPS sizer, CPC, and other aerosol instruments to do in-situ aerosol monitoring at Doi Ang Khang mountain, north of Thailand (19.93˚N，99.05˚E，1536m) and Lulin Mountain, Taiwan (23.47˚N，120.87˚E，2862m), then analyzed biomass burning aerosol properties and aerosol activation properties according to the data from these instruments. The observation time is during 2/22~4/8 2013. This period is Thailand's dry (spring) season, and this area occurred biomass burning events continually. By backward trajectory path analysis, we found that different air source’s aerosol properties have considerable variations, and we can classify into three events. The first event, A, is during 3/13~15. In this event, the impact of overseas transport and biomass burning showed the better hygroscopic and high activation ratio. The second event, B, is during 3/17~20, because the affection of biomass burning is serious and the biggest in these three events, so the hygroscopic and activation ratio decreased. The third event, C, is during 3/22~24, the air mass transportation is above the boundary layer. This study speculates that due to aerosol aging, so the hygroscopic and activation ratio are the lowest.

Lulin station located on the downstream of Indochina and China, and we found the trajectory of air mass pass through the artificially pollution area in China, and the biomass burning source regions in Indochina, so we speculated aerosol properties will affect by the trajectory of air mass. In this study, we classified into three events, too. The first event, I, is during 3/13~15. According to the result of the backward trajectory, we found that the aerosol property will be affected by biomass burning source region, showing the low hygroscopic and activation ratio. The second event, II, is during 3/16 ~18. Its air mass transportation is passed through the northeast of China, Korea, Japan and other regions, so the aerosol property will be affected by artificially pollution. The third event, III, is during 3/19~20. This event is similar to event I, but the degree of pollution is stronger.

Overall, the different source region and the influence of transported path will cause the more variations of the aerosol properties, and the result of the downstream test shows different property between these two regions. Combining these into results, the research of Indochina artificial activities will be completed and the influence of Cloud Condensation Nuclei (CCN) will also be clearly in this study.

Reference ( 110 ) 〈TOP〉

Abel, S. J., Haywood, J. M., Highwood, E. J., Li, J., and Buseck, P. R. (2003). Evolution of biomass burning aerosol properties from an agricultural fire in southern Africa. Geophysical Research Letters 30.
連結：
Ackerman, A. S., Kirkpatrick, M. P., Stevens, D. E., and Toon, O. B. (2004). The impact of humidity above stratiform clouds on indirect aerosol climate forcing. Nature 432, 1014-1017.
連結：
Adler, G., Flores, J., Abo Riziq, A., Borrmann, S., and Rudich, Y. (2011). Chemical, physical, and optical evolution of biomass burning aerosols: a case study. Atmospheric Chemistry and Physics 11, 1491-1503.
連結：
Albrecht, B. A. (1989). Aerosols, cloud microphysics, and fractional cloudiness. Science 245, 1227-1230.
連結：
Andreae, M., and Rosenfeld, D. (2008). Aerosol–cloud–precipitation interactions. Part 1. The nature and sources of cloud-active aerosols. Earth-Science Reviews 89, 13-41.
連結：

Times Cited (1) 〈TOP〉

蔡茗宇(2014)。2013年春季鹿林山和夏季龍潭氣膠水溶性離子短時間動態變化特性。中央大學環境工程研究所學位論文。2014。1-329。

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