Aerosol physical and chemical properties retrieved from ground-based remote sensing measurements during heavy haze days in Beijing winter

被引:172
作者
Li, Z. [1 ]
Gu, X. [1 ]
Wang, L. [1 ,2 ]
Li, D. [1 ,3 ]
Xie, Y. [1 ,3 ]
Li, K. [1 ,3 ]
Dubovik, O. [4 ]
Schuster, G.
Goloub, P. [4 ]
Zhang, Y. [1 ,3 ]
Li, L. [1 ,3 ]
Ma, Y. [1 ]
Xu, H. [1 ]
机构
[1] Chinese Acad Sci, Inst Remote Sensing & Digital Earth, State Environm Protect Key Lab Satellites Remote, Beijing 100101, Peoples R China
[2] Nanjing Univ, Int Inst Earth Syst Sci, Nanjing 210093, Jiangsu, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[4] Univ Lille 1, Opt Atmospher Lab, F-59655 Villeneuve Dascq, France
基金
中国国家自然科学基金;
关键词
URBAN AIR-POLLUTION; LIGHT-ABSORPTION; BLACK CARBON; ATMOSPHERIC AEROSOLS; OPTICAL-PROPERTIES; ANGSTROM EXPONENT; AERONET; VISIBILITY; PARTICLES; CHINA;
D O I
10.5194/acp-13-10171-2013
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
With the increase in economic development over the past thirty years, many large cities in eastern and southwestern China are experiencing increased haze events and atmospheric pollution, causing significant impacts on the regional environment and even climate. However, knowledge on the aerosol physical and chemical properties in heavy haze conditions is still insufficient. In this study, two winter heavy haze events in Beijing that occurred in 2011 and 2012 were selected and investigated by using the ground-based remote sensing measurements. We used a CIMEL CE318 sun-sky radiometer to retrieve haze aerosol optical, physical and chemical properties, including aerosol optical depth (AOD), size distribution, complex refractive indices and aerosol fractions identified as black carbon (BC), brown carbon (BrC), mineral dust (DU), ammonium sulfate-like (AS) components and aerosol water content (AW). The retrieval results from a total of five haze days showed that the aerosol loading and properties during the two winter haze events were comparable. Therefore, average heavy haze property parameters were drawn to present a research case for future studies. The average AOD is about 3.0 at 440 nm, and the Angstrom exponent is 1.3 from 440 to 870 nm. The fine-mode AOD is 2.8 corresponding to a fine-mode fraction of 0.93. The coarse particles occupied a considerable volume fraction of the bimodal size distribution in winter haze events, with the mean particle radius of 0.21 and 2.9 mu m for the fine and coarse modes respectively. The real part of the refractive indices exhibited a relatively flat spectral behavior with an average value of 1.48 from 440 to 1020 nm. The imaginary part showed spectral variation, with the value at 440 nm (about 0.013) higher than the other three wavelengths (about 0.008 at 675 nm). The aerosol composition retrieval results showed that volume fractions of BC, BrC, DU, AS and AW are 1, 2, 49, 15 and 33 %, respectively, on average for the investigated haze events. The preliminary uncertainty estimation and comparison of these remote sensing results with in situ BC and PM2.5 measurements are also presented in the paper.
引用
收藏
页码:10171 / 10183
页数:13
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