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首页> 外文期刊>Atmospheric Measurement Techniques >Estimation of aerosol complex refractive indices for both fine and coarse modes simultaneously based on AERONET remote sensing products
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Estimation of aerosol complex refractive indices for both fine and coarse modes simultaneously based on AERONET remote sensing products

机译:基于AERONET遥感产品同时估算精细模式和粗糙模式的气溶胶复折射率

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Climate change assessment, especially model evaluation, requires a better understanding of complex refractive indices (CRIs) of atmospheric aerosols – separately for both fine and coarse modes. However, the widely used aerosol CRI obtained by the global Aerosol Robotic Network (AERONET) corresponds to total-column aerosol particles without separation for fine and coarse modes. This paper establishes a method to separate CRIs of fine and coarse particles based on AERONET volume particle size distribution (VPSD), aerosol optical depth (AOD) and absorbing AOD (AAOD). The method consists of two steps. First a multimodal log-normal distribution that best approximates the AERONET VPSD is found. Then the fine and coarse mode CRIs are found by iterative fitting of AERONET AODs to Mie calculations. The numerical experiment shows good performance for typical water-soluble, biomass burning and dust aerosol types, and the estimated uncertainties on the retrieved sub-mode CRIs are about 0.11 (real part) and 78?% (imaginary part). The 1-year measurements at the AERONET Beijing site are processed, and we obtain CRIs of 1.48–0.010ii/i (imaginary part at 440?nm is 0.012) for fine mode particles and 1.49–0.004ii/i (imaginary part at 440?nm is 0.007) for coarse mode particles, for the period of 2014–2015. Our results also suggest that both fine and coarse aerosol mode CRIs have distinct seasonal characteristics; in particular, CRIs of fine particles in winter season are significantly higher than summer due to possible anthropogenic influences.
机译:气候变化评估,尤其是模型评估,需要更好地了解大气气溶胶的复折射率(CRI)–分别针对精细模式和粗糙模式。但是,全球气溶胶机器人网络(AERONET)获得的广泛使用的气溶胶CRI对应于没有分离的细颗粒和粗颗粒的总气溶胶颗粒。本文建立了一种基于AERONET体积粒径分布(VPSD),气溶胶光学深度(AOD)和吸收AOD(AAOD)分离细颗粒和粗颗粒CRI的方法。该方法包括两个步骤。首先,找到最接近AERONET VPSD的多峰对数正态分布。然后,通过将AERONET AOD迭代拟合到Mie计算中,找到精细模式CRI和粗糙模式CRI。数值实验表明,对于典型的水溶性,生物质燃烧和粉尘气溶胶类型,具有良好的性能,并且所取回的子模式CRI的估计不确定性约为0.11(实部)和78%(虚部)。处理了AERONET北京站点的1年测量结果,对于细模粒子,我们获得的CRI为1.48–0.010 i (在440?nm处的虚部为0.012)和1.49–0.004 2014年至2015年期间,粗模式粒子的i(在440?nm处的虚部为0.007)。我们的结果还表明,精细和粗糙的气溶胶模式CRI都有明显的季节性特征。特别是由于可能的人为影响,冬季的细颗粒CRI明显高于夏季。

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