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首页> 外文期刊>Atmospheric chemistry and physics >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
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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

机译:2000年至2010年中国精细模式MODIS气溶胶光学深度的年际变化及其与二氧化硫排放量变化的关系

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Anthropogenic SO2 emissions increased alongside economic development inChina at a rate of 12.7% yr?1 from 2000 to 2005. However, under new Chinesegovernment policy, SO2 emissions declined by 3.9% yr?1 between 2005 and2009. Between 2000 and 2010, we found that the variability in the fine-mode(submicron) aerosol optical depth (AOD) over the oceans adjacent to East Asiaincreased by 3–8% yr?1 to a peak around 2005–2006 and subsequently decreasedby 2–7% yr?1, based on observations by the Moderate Resolution ImagingSpectroradiometer (MODIS) on board NASA's Terra satellite and simulations bya chemical transport model. This trend is consistent with ground-basedobservations of aerosol particles at a mountainous background observationsite in central Japan. These fluctuations in SO2 emission intensity andfine-mode AOD are thought to reflect the widespread installation of fuel-gasdesulfurization (FGD) devices in power plants in China, because aerosolsulfate is a major determinant of the fine-mode AOD in East Asia. Using achemical transport model, we confirmed that the contribution of particulatesulfate to the fine-mode AOD is more than 70% of the annual mean and thatthe abovementioned fluctuation in fine-mode AOD is caused mainly by changesin SO2 emission rather than by other factors such as varyingmeteorological conditions in East Asia. A strong correlation was also foundbetween satellite-retrieved SO2 vertical column density and bottom-upSO2 emissions, both of which were also consistent with observed fine-modeAOD trends. We propose a simplified approach for evaluating changes in SO2emissions in China, combining the use of modeled sensitivity coefficientsthat describe the variation of fine-mode AOD with changes in SO2 emissionsand satellite retrieval. Satellite measurements of fine-mode AOD above theSea of Japan marked a 4.1% yr?1 decline between 2007 and 2010, whichcorresponded to the 9% yr?1 decline in SO2 emissions from China during thesame period.
机译:2000年至2005年,人为排放的SO 2 随经济发展而增长,增长率为12.7%yr 1 。但是,在新的中国政府政策下,SO 2 < / sub>排放量在2005年至2009年间下降了3.9%yr 1 。在2000年至2010年之间,我们发现与东亚相邻的海洋的细模(亚微米)气溶胶光学深度(AOD)的变化增加了3-8%yr ?1 ,达到了一个峰值基于NASA Terra卫星上的中等分辨率成像光谱仪(MODIS)的观测结果以及化学传输模型的模拟结果,2005-2006年和随后减少了2%-7%yr 1 。这种趋势与日本中部山区背景观测站点对气溶胶颗粒的地面观测是一致的。 SO 2 排放强度和精细模式AOD的这些波动被认为反映了中国发电厂中广泛安装的燃料脱硫(FGD)装置,因为气溶胶硫酸盐是精细模式的主要决定因素。东亚地区的AOD。使用化学迁移模型,我们确认了硫酸盐对精细模式AOD的贡献超过年均值的70%,并且上述精细模式AOD的波动主要是由SO 2 的变化引起的排放,而不是受其他因素(例如东亚气象条件的变化)的影响。卫星获取的SO 2 垂直列密度与自下而上的SO 2 排放之间也存在很强的相关性,这两者都与观测到的精细模式AOD趋势一致。我们提出了一种简化的方法来评估中国SO 2 的排放量,并结合使用模型灵敏度系数来描述精细模式AOD的变化与SO 2 排放量的变化。卫星检索。在日本海上空进行的精细模式AOD的卫星测量表明,2007年至2010年yr ?1 下降了4.1%,与SO sup>?1 下降了9%同期来自中国的sub> 2 排放。

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