Atmos. Chem. Phys., 12, 2631-2640, 2012
www.atmos-chem-phys.net/12/2631/2012/
doi:10.5194/acp-12-2631-2012
© Author(s) 2012. This work is distributed
under the Creative Commons Attribution 3.0 License.
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
S. Itahashi1, I. Uno2, K. Yumimoto3, H. Irie4, K. Osada5, K. Ogata6, H. Fukushima6, Z. Wang7, and T. Ohara8
1Department of Earth System Science and Technology, Kyushu University, Fukuoka, Japan
2Research Institute for Applied Mechanics, Kyushu University, Fukuoka, Japan
3Meteorological Research Institute, Tsukuba, Ibaraki, Japan
4Research Institute for Global Change, JAMSTEC, Yokohama, Japan
5Graduate School of Environmental Sciences, Nagoya University, Nagoya, Japan
6School of High-Technology for Human Welfare, Tokai University, Numazu, Japan
7State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
8National Institute for Environmental Studies, Tsukuba, Ibaraki, Japan

Abstract. 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.

Citation: Itahashi, S., Uno, I., Yumimoto, K., Irie, H., Osada, K., Ogata, K., Fukushima, H., Wang, Z., and Ohara, T.: 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, Atmos. Chem. Phys., 12, 2631-2640, doi:10.5194/acp-12-2631-2012, 2012.
 
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