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Aircraft measurements of the vertical distribution and activation property of aerosol particles over the Loess Plateau in China

机译:黄土高原地区气溶胶颗粒垂直分布和活化特性的飞机测量

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摘要

For the first time, comprehensive aircraft measurements of atmospheric aerosols and cloud condensation nuclei (CCN) were made over the Loess Plateau in Shanxi, China. Data from six flights in July and August 2013 were analyzed. Fine aerosols were predominant over the region. On the one hazy day, the fraction of fine particles in the total aerosol load was the greatest. Aerosol number concentration decreased exponentially with altitude. Inversion layers caused low-level aerosol accumulation zones. The mean aerosol particle size increased with altitude, and the larger particles were mainly found above 2 km. Aerosol number size distributions at different height ranges showed two or three peaks. The aerosol number size distribution from 0.01 μm to 20 μm can be fitted with three log-normal distribution functions. The number concentration of CCN (N_(CCN)) decreased with altitude. N_(CCN) was linearly related to the CN concentration (N_(CN)). The fraction of CCN to CN (f_(CCN/CN)) at 0.3% SS was half of that at 0.4% SS. The f_(CCN/CN) on the hazy day was lower than on the clear days. Vertical profiles of f_(CCN/CN) and the effective diameter (ED) were similar, although the f_(CCN/CN) increased with altitude.
机译:首次在中国山西黄土高原进行了飞机大气气溶胶和云凝结核(CCN)的综合测量。分析了2013年7月和2013年8月的六个航班的数据。优良的气溶胶在该地区占主导地位。在雾霾的第一天,细颗粒在总气溶胶负荷中所占的比例最大。气溶胶浓度随海拔高度呈指数下降。逆转层引起低水平的气溶胶聚集区。平均气溶胶粒径随海拔升高而增大,较大的气溶胶粒径主要在2 km以上。在不同高度范围内的气溶胶数大小分布显示两个或三个峰值。从0.01μm到20μm的气溶胶数大小分布可以拟合三个对数正态分布函数。 CCN(N_(CCN))的浓度随着海拔的升高而降低。 N_(CCN)与CN浓度(N_(CN))呈线性关系。 SS在0.3%SS时占CN的比例(f_(CCN / CN))是0.4%SS时的一半。雾天的f_(CCN / CN)低于晴天。尽管f_(CCN / CN)随高度增加,但f_(CCN / CN)和有效直径(ED)的垂直轮廓相似。

著录项

  • 来源
    《Atmospheric research 》 |2015年第3期| 73-86| 共14页
  • 作者单位

    Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, School of Atmospheric Physics, Nanjing University of Information Science and Technology, Nanjing, Jiangsu 210044, China,Weather Modification Office of Shanxi Province, Taiyuan, Shanxi 030032, China;

    Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, School of Atmospheric Physics, Nanjing University of Information Science and Technology, Nanjing, Jiangsu 210044, China,Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, Nanjing, Jiangsu 210044, China;

    Weather Modification Office of Shanxi Province, Taiyuan, Shanxi 030032, China;

    College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China,Department of Atmospheric and Oceanic Science and Earth System Science Interdisciplinary Center (ESSIC) University of Maryland, College Park MD, USA;

    College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China;

    Department of Atmospheric and Oceanic Science and Earth System Science Interdisciplinary Center (ESSIC) University of Maryland, College Park MD, USA;

    College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China,Meteorological Institute of Shaanxi Province, Xi'an, Shaanxi 710017, China;

    College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China;

    Meteorological Station in Anhui Province, Hefei, Anhui 230031, China;

    Weather Modification Office of Shanxi Province, Taiyuan, Shanxi 030032, China;

    Weather Modification Office of Shanxi Province, Taiyuan, Shanxi 030032, China;

    Weather Modification Office of Shanxi Province, Taiyuan, Shanxi 030032, China;

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

    Vertical distribution; Size distribution; Activation property; Aircraft measurements; The Loess Plateau;

    机译:垂直分布;尺寸分布;激活属性;飞机尺寸黄土高原;

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