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石家庄秋季大气气溶胶物理特征分析 被引量:29

The Analysis of Physical Feature of Aerosol Particles in Autumn over Shijiazhuang Area
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摘要 利用1990年秋季在石家庄地区不同天气条件下飞机观测对流层低层(距地面4000m以下高度)大气气溶胶的观测资料,分析了气溶胶粒子数密度、质量浓度水平和垂直分布特征及其日变化。结果表明,晴空下,石家庄地区气溶胶源于本地,地面质量浓度为0.15×10-9—0.85×10-9·cm-3,高度4000m以下谱分布特征值逆温层影响气溶胶粒子的向上输送,使其在送温层上下出现不连续分布;气溶胶的日变化表现为上午数密度大于下午,但下午粒子谱变宽;城市效应影响气溶胶粒子分布,城市上空气溶胶粒子数密度比郊区高15%-30%。 The daily change of number density of aerosol particles and quality concentration in horizontal and vertical derection are analyzed. The earosol data observated by aircraft is used in convective baundary layer under different weather conditions during autumn in 1990 over shijiazhuang area. The results show that the aerosol particles are of local ones under clear air over shijiazhuang area. The concentration of aerosol particles is from 0. 15 ×10-9 to 0. 85 ×10-g. cm-3. The characteristic value of spectral distribution N0 is from 1. 5 ×105 to 5. 5 ×105g. cm-3,and λ value is from 13 to 15μm-1 below 4000 meters. The upward transport of aerosol particles is limited,and its distribution occurred discontinuity due to the inversion layer effected.The daily change of aerosol number density in the morning was greater than in the afternoon. The spectral distrbution of aerosol particles was affected for the city effected. The number density of aerosol particles over the city area was higher than that over the rural area.
出处 《气象》 CSCD 北大核心 1996年第2期40-43,共4页 Meteorological Monthly
基金 河北省科学基金 中国气象局科学基金
关键词 气溶胶 分布特征 大气 物理特征 aerosol particle number density quality concentration distribution character
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参考文献3

  • 1游来光,云降水物理和人工增雨技术研究,1994年
  • 2谷福印,环境科学学报,1989年,9卷
  • 3陈万奎,环境科学学报,1985年,5卷,3期

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