Interannual variation in the fine-mode MODIS aerosol optical depth and its relationship to the changes in sulfur dioxide emissions in China between 2000 and 2010

被引:49
作者
Itahashi, S. [1 ]
Uno, I. [2 ]
Yumimoto, K. [3 ]
Irie, H. [4 ]
Osada, K. [5 ]
Ogata, K. [6 ]
Fukushima, H. [6 ]
Wang, Z. [7 ]
Ohara, T. [8 ]
机构
[1] Kyushu Univ, Dept Earth Syst Sci & Technol, Fukuoka 8168580, Japan
[2] Kyushu Univ, Appl Mech Res Inst, Fukuoka 8168580, Japan
[3] Meteorol Res Inst, Tsukuba, Ibaraki 305, Japan
[4] JAMSTEC, Res Inst Global Change, Yokohama, Kanagawa, Japan
[5] Nagoya Univ, Grad Sch Environm Sci, Nagoya, Aichi 4648601, Japan
[6] Tokai Univ, Sch High Technol Human Welf, Numazu, Japan
[7] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Atmospher Boundary Layer Phys & Atm, Beijing, Peoples R China
[8] Natl Inst Environm Studies, Tsukuba, Ibaraki, Japan
基金
日本学术振兴会;
关键词
EAST-ASIA; RISHIRI ISLAND; ACE-ASIA; PARTICLES; TRENDS;
D O I
10.5194/acp-12-2631-2012
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Anthropogenic SO2 emissions increased alongside economic development in China at a rate of 12.7% yr(-1) from 2000 to 2005. However, under new Chinese government policy, SO2 emissions declined by 3.9% yr(-1) between 2005 and 2009. Between 2000 and 2010, we found that the variability in the fine-mode (submicron) aerosol optical depth (AOD) over the oceans adjacent to East Asia increased by 3-8% yr(-1) to a peak around 2005-2006 and subsequently decreased by 2-7% yr(-1), based on observations by the Moderate Resolution Imaging Spectroradiometer (MODIS) on board NASA's Terra satellite and simulations by a chemical transport model. This trend is consistent with ground-based observations of aerosol particles at a mountainous background observation site in central Japan. These fluctuations in SO2 emission intensity and fine-mode AOD are thought to reflect the widespread installation of fuel-gas desulfurization (FGD) devices in power plants in China, because aerosol sulfate is a major determinant of the fine-mode AOD in East Asia. Using a chemical transport model, we confirmed that the contribution of particulate sulfate to the fine-mode AOD is more than 70% of the annual mean and that the abovementioned fluctuation in fine-mode AOD is caused mainly by changes in SO2 emission rather than by other factors such as varying meteorological conditions in East Asia. A strong correlation was also found between satellite-retrieved SO2 vertical column density and bottom-up SO2 emissions, both of which were also consistent with observed fine-mode AOD trends. We propose a simplified approach for evaluating changes in SO2 emissions in China, combining the use of modeled sensitivity coefficients that describe the variation of fine-mode AOD with changes in SO2 emissions and satellite retrieval. Satellite measurements of fine-mode AOD above the Sea of Japan marked a 4.1% yr(-1) decline between 2007 and 2010, which corresponded to the 9% yr(-1) decline in SO2 emissions from China during the same period.
引用
收藏
页码:2631 / 2640
页数:10
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