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Aerosol optical properties in the Arctic: The role of aerosol chemistry and dust composition in a closure experiment between Lidar and tethered balloon vertical profiles

机译:北极的气溶胶光学性质:气溶胶化学和粉尘成分在激光雷达与系留气球垂直剖面之间的封闭实验中的作用

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摘要

A closure experiment was conducted over Svalbard by comparing Lidar measurements and optical aerosol properties calculated from aerosol vertical profiles measured using a tethered balloon. Arctic Haze was present together with Icelandic dust. Chemical analysis of filter samples, aerosol size distribution and a full set of meteorological parameters were determined at ground. Moreover, scanning electron microscopy coupled with energy-dispersive X-ray (SEM-EDS) data were at disposal showing the presence of several mineralogical phases (i.e., sheet silicates, gypsum, quartz, rutile, hematite).The closure experiment was set up by calculating the backscattering coefficients from tethered balloon data and comparing them with the corresponding lidar profiles. This was preformed in three subsequent steps aimed at determining the importance of a complete aerosol speciation: (i) a simple, columnar refractive index was obtained by the closest Aerosol Robotic Network (AERONET) station, (ii) the role of water-soluble components, elemental carbon and organic matter (EC/OM) was addressed, (iii) the dust composition was included.When considering the AERONET data, or only the ionic water-soluble components and the EC/OM fraction, results showed an underestimation of the backscattering lidar signal up to 76, 53 and 45% (355, 532 and 1064 nm). Instead, when the dust contribution was included, the underestimation disappeared and the vertically-averaged, backscattering coefficients (1.45 +/- 0.30. 0.69 +/- 0.15 and 0.34 +/- 0.08 Mm(-1) sr(-1), at 355, 532 and 1064 nm) were found in keeping with the lidar ones (1.60 +/- 0.22, 0.75 +/- 0.16 and 0.31 +/- 0.08 Mm(-1) sr(-1)). Final results were characterized by low RMSE (0.36, 0.08 and 0.04 Mm(-1) sr(-1)) and a high linear correlation (R-2 of 0.992, 0.992 and 0.994) with slopes close to one (1.368,0.931 and 0.977, respectively). This work highlighted the importance of all the aerosol components and of the synergy between single particle and bulk chemical analysis for the optical property characterization in the Arctic. (C) 2019 Elsevier B.V. All rights reserved.
机译:通过比较激光雷达测量值和光学气溶胶特性,在斯瓦尔巴群岛进行了封闭实验,光学气溶胶特性是根据使用系留气球测得的气溶胶垂直剖面计算得出的。北极阴霾与冰岛的灰尘一起出现。在地面确定了过滤器样品的化学分析,气溶胶尺寸分布和全套气象参数。此外,扫描电子显微镜与能量色散X射线(SEM-EDS)数据结合使用,表明存在几种矿物学相(即片状硅酸盐,石膏,石英,金红石,赤铁矿)。建立了封闭实验通过根据系留气球数据计算后向散射系数,并将其与相应的激光雷达轮廓进行比较。这是在随后的三个步骤中执行的,这些步骤旨在确定完整的气溶胶形态的重要性:(i)最近的气溶胶机器人网络(AERONET)站获得了简单的柱状折射率,(ii)水溶性成分的作用,元素碳和有机物(EC / OM),(iii)包括粉尘成分。当考虑AERONET数据或仅考虑离子型水溶性成分和EC / OM分数时,结果表明低估了激光雷达后向散射信号高达76、53和45%(355、532和1064 nm)。相反,当包括灰尘贡献时,低估消失并且垂直平均后向散射系数(1.45 +/- 0.30。0.69 +/- 0.15和0.34 +/- 0.08 Mm(-1)sr(-1)在355、532和1064 nm)与激光雷达(1.60 +/- 0.22、0.75 +/- 0.16和0.31 +/- 0.08 Mm(-1)sr(-1)一致)。最终结果的特点是RMSE低(0.36、0.08和0.04 Mm(-1)sr(-1))和高线性相关性(R-2为0.992、0.992和0.994),斜率接近于1(1.368、0.931和分别为0.977)。这项工作强调了所有气溶胶成分的重要性,以及单个颗粒与大块化学分析之间协同作用对于北极光学特性表征的重要性。 (C)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《The Science of the Total Environment》 |2019年第10期|452-467|共16页
  • 作者单位

    Univ Milano Bicocca, GEMMA Res Ctr, Dept Earth & Environm Sci, Piazza Sci 1, I-20126 Milan, Italy|Univ Milano Bicocca, POLARIS Res Ctr, Dept Earth & Environm Sci, Piazza Sci 1, I-20126 Milan, Italy;

    Alfred Wegener Inst Polar & Meeresforsch AWI, Forsch Stelle Potsdam, Telegraphenberg 4311, D-14473 Potsdam, Germany;

    Univ Perugia, Dept Chem Biol & Biotecnol, Via Elce di Sotto 8, I-06123 Perugia, Italy|CNR, Inst Atmospher Sci & Climate, CNR ISAC, Via P Gobetti 101, I-40129 Bologna, Italy;

    Univ Perugia, Dept Chem Biol & Biotecnol, Via Elce di Sotto 8, I-06123 Perugia, Italy;

    Jozef Stefan Inst, Dept Condensed Matter Phys, Jamova 39, SI-1000 Ljubljana, Slovenia;

    CNR, Inst Atmospher Sci & Climate, CNR ISAC, Via P Gobetti 101, I-40129 Bologna, Italy;

    CNR, Inst Atmospher Sci & Climate, CNR ISAC, Via P Gobetti 101, I-40129 Bologna, Italy;

    CNR, Inst Atmospher Sci & Climate, CNR ISAC, Via P Gobetti 101, I-40129 Bologna, Italy|Univ Florence, Dept Chem, Via Lastruccia 3, I-50019 Florence, Italy;

    CNR, Inst Atmospher Sci & Climate, CNR ISAC, Via P Gobetti 101, I-40129 Bologna, Italy|Univ Florence, Dept Chem, Via Lastruccia 3, I-50019 Florence, Italy;

    Univ Milano Bicocca, GEMMA Res Ctr, Dept Earth & Environm Sci, Piazza Sci 1, I-20126 Milan, Italy|Univ Milano Bicocca, POLARIS Res Ctr, Dept Earth & Environm Sci, Piazza Sci 1, I-20126 Milan, Italy;

    Alfred Wegener Inst Polar & Meeresforsch AWI, Forsch Stelle Potsdam, Telegraphenberg 4311, D-14473 Potsdam, Germany;

    CNR, Inst Atmospher Sci & Climate, CNR ISAC, Via P Gobetti 101, I-40129 Bologna, Italy;

    Univ Milano Bicocca, GEMMA Res Ctr, Dept Earth & Environm Sci, Piazza Sci 1, I-20126 Milan, Italy|Univ Milano Bicocca, POLARIS Res Ctr, Dept Earth & Environm Sci, Piazza Sci 1, I-20126 Milan, Italy;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Aerosol; Svalbard; Optical properties; Back scattering; Chemical composition; Icelandic dust; Lidar;

    机译:气溶胶;Svalbard;光学性质;背部散射;化学成分;冰岛尘埃;延裙;

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