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Multi-wavelength Raman lidar, sun photometric and aircraft measurements in combination with inversion models for the estimation of the aerosol optical and physico-chemical properties over Athens, Greece

机译:多波长拉曼激光雷达,太阳光度法和飞机测量与反演模型相结合,用于估计希腊雅典上空的气溶胶光学和物理化学性质

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摘要

A novel procedure has been developed to retrieve, simultaneously, theoptical, microphysical and chemical properties of tropospheric aerosols witha multi-wavelength Raman lidar system in the troposphere over an urban site(Athens, Greece: 37.9° N, 23.6° E, 200 m a.s.l.) using data obtainedduring the European Space Agency (ESA) THERMOPOLIS project, which took placebetween 15–31 July 2009 over the Greater Athens Area (GAA). We selected toapply our procedure for a case study of intense aerosol layers that occurred on20–21 July 2009. The National Technical University of Athens (NTUA) EOLE6-wavelength Raman lidar system has been used to provide the verticalprofiles of the optical properties of aerosols (extinction and backscattercoefficients, lidar ratio) and the water vapor mixing ratio. An inversionalgorithm was used to derive the mean aerosol microphysical properties (meaneffective radius (), single-scattering albedo ) and mean complexrefractive index ()) at selected heights in the 2–3 km height region. Wefound that was 0.14–0.4 (±0.14) μm, ω was 0.63–0.88 (±0.08)(at 532 nm) and ranged from 1.44 (±0.10) + 0.01 (±0.01) to1.55 (±0.12) + 0.06 (±0.02), in good agreement (only for the values) with in situ aircraft measurements. The water vapor and temperatureprofiles were incorporated into the ISORROPIA II model to propose a possiblein situ aerosol composition consistent with the retrieved and values. Theretrieved aerosol chemical composition in the 2–3 km height region gave avariable range of sulfate (0–60%) and organic carbon (OC) content(0–50%), although the OC content increased (up to 50%) and the sulfatecontent dropped (up to 30%) around 3 km height; the retrieved low value (0.63), indicates the presence of absorbing biomass burning smokemixed with urban haze. Finally, the retrieved aerosol microphysicalproperties were compared with column-integrated sun photometer CIMEL data.
机译:已开发出一种新颖的程序来同时在城市对流层中利用对流层中的多波长拉曼激光雷达系统检索对流层气溶胶的光学,微物理和化学性质(希腊雅典:37.9°N,23.6°E,200 m升)使用的数据来自欧洲航天局(ESA)THERMOPOLIS项目,该项目于2009年7月15日至31日在大雅典地区(GAA)进行。我们选择将程序应用于2009年7月20日至21日发生的强烈气溶胶层的案例研究。雅典国立技术大学(NTUA)的EOLE6波长拉曼激光雷达系统已用于提供气溶胶光学特性的垂直剖面图(消光系数和反向散射系数,激光雷达比)和水蒸气混合比。在2至3 km高度区域内选定的高度,使用反演算法来推导平均气溶胶微物理性质(平均有效半径(),单散射反照率)和平均复数折射率())。我们发现其为0.14–0.4(±0.14)μm,ω为0.63–0.88(±0.08)(在532 nm处),范围从1.44(±0.10)+ 0.01(±0.01)到1.55(±0.12)+ 0.06( (±0.02),与飞机原位测量值非常吻合(仅适用于数值)。将水蒸气和温度曲线合并到ISORROPIA II模型中,以提出可能与恢复值和值一致的可能的原位气溶胶成分。尽管OC含量增加(高达50%),而OC含量增加(高达50%),但在2-3 km高的区域气溶胶化学成分给出了硫酸盐(0-60%)和有机碳(OC)含量(0-50%)的可变范围。硫酸盐含量在3 km高处下降(高达30%);检索到的低值(0.63)表示存在吸收燃烧的生物量的烟气并混有城市霾。最后,将检索到的气溶胶微物理性质与柱积分太阳光度计CIMEL数据进行比较。

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