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中国农学通报 ›› 2016, Vol. 32 ›› Issue (11): 167-176.doi: 10.11924/j.issn.1000-6850.casb15120173

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

晴空条件下华北平原城市气溶胶观测个例分析

胡向峰,段宇辉,孙玉稳,吴志会,董晓波   

  1. 河北省人工影响天气办公室,河北省气象台,河北省人工影响天气办公室,河北省人工影响天气办公室,河北省人工影响天气办公室
  • 收稿日期:2015-12-31 修回日期:2016-01-18 接受日期:2016-01-22 出版日期:2016-04-20 发布日期:2016-04-20
  • 通讯作者: 胡向峰
  • 基金资助:
    河北省科技支撑计划项目“河北省旱季人工增雨(雪)防灾减灾关键技术研究”(11277107D);公益性行业(气象)科研专项“层状云人工增雨作业条件识别和效果分析技术”(GYHY201206003)。

Aerosol Observation in Cities of North China Plain Under Clear Day Condition

  • Received:2015-12-31 Revised:2016-01-18 Accepted:2016-01-22 Online:2016-04-20 Published:2016-04-20

摘要: 为了探讨气溶胶污染的微观特征及可能原因,利用2008 年10 月19 日一次飞机探测的资料,对保定和石家庄的气溶胶分布特征进行对比分析。结果发现:保定边界层内气溶胶数浓度垂直递减明显,边界层以上接近背景气溶胶。石家庄边界层附近气溶胶浓度出现累积,边界层以上数浓度迅速降低,2300 m出现峰值。逆温层和相对湿度峰值附近累积的较高浓度的气溶胶是影响气溶胶垂直分布的重要原因。气溶胶数浓度和平均直径与相对湿度并不完全呈正相关。1500 m以下气溶胶浓度与局地排放源有直接关系,人为活动及风速是影响气溶胶水平分布的重要因素。区域输送对混合层以上气溶胶浓度的影响较大。保定不同高度层的粒子谱均呈单峰分布,石家庄低层粒子谱呈双峰或三峰分布。

关键词: 干旱灾害, 干旱灾害, 风险指数, 区划, 洪洞县

Abstract: In order to find the possible causes and micro characteristics of aerosol pollution, based on the airplane detection data on Oct 19th, 2008, the aerosol distribution characteristics over Baoding and Shijiazhuang were contrasted and analyzed. The results showed that: the aerosol number concentration declined obviously under boundary layer, and approached background concentration of aerosol above boundary layer. The aerosol number concentration was accumulated near the boundary layer over Shijiazhuang, declined rapidly above the boundary layer, presented a peak value at the height of 2300 m. There were different vertical distribution characteristics near the boundary layer top. The inversion layer and relative humidity had a great impact on the vertical distribution of aerosol. The number concentration and mean diameter did not completely and positively correlate with relative humidity. The aerosol number concentration was directly related with regional emission sources below 1500 m, human activities and wind speed were important factors influencing the horizontal distribution of aerosol. The aerosol number concentration above mixed layer was mainly affected by regional transport. The aerosol particle spectrum at different height levels presented unimodal pattern over Baoding and bimodal or three-modal pattern at lower levels over Shijiazhuang.

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