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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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摘要

Climate change assessment, especially model evaluation, requires a betterunderstanding of complex refractive indices (CRIs) of atmospheric aerosols –separately for both fine and coarse modes. However, the widely used aerosolCRI obtained by the global Aerosol Robotic Network (AERONET) corresponds tototal-column aerosol particles without separation for fine and coarse modes.This paper establishes a method to separate CRIs of fine and coarse particlesbased on AERONET volume particle size distribution (VPSD), aerosol opticaldepth (AOD) and absorbing AOD (AAOD). The method consists of two steps. Firsta multimodal log-normal distribution that best approximates the AERONET VPSDis found. Then the fine and coarse mode CRIs are found by iterative fittingof AERONET AODs to Mie calculations. The numerical experiment shows goodperformance for typical water-soluble, biomass burning and dust aerosoltypes, and the estimated uncertainties on the retrieved sub-mode CRIs areabout 0.11 (real part) and 78 % (imaginary part). The 1-year measurementsat the AERONET Beijing site are processed, and we obtain CRIs of1.48–0.010 (imaginary part at 440 nm is 0.012) for fine mode particlesand 1.49–0.004 (imaginary part at 440 nm is 0.007) for coarse modeparticles, for the period of 2014–2015. Our results also suggest that bothfine and coarse aerosol mode CRIs have distinct seasonal characteristics; inparticular, CRIs of fine particles in winter season are significantly higherthan summer due to possible anthropogenic influences.
机译:气候变化评估,尤其是模型评估,需要更好地理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aerosolCRI对应于无需分离细颗粒和粗颗粒模式的总气溶胶颗粒。本文建立了一种基于AERONET体积粒径分布分离细颗粒和粗颗粒CRI的方法( VPSD),气溶胶光学深度(AOD)和吸收性AOD(AAOD)。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计算中来找到精细模式CRI和粗模式CRI。数值实验表明,该方法对典型的水溶性,生物质燃烧和粉尘气溶胶类型具有良好的性能,并且所获得的亚模式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(440 nm处的虚部为0.012),对于粗模粒子,其CRI为1.49–0.004(440 nm处的虚部为0.007), 2014-2015年期间。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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