首页 | 官方网站   微博 | 高级检索  
     

京津冀区域典型重污染过程与反馈效应研究
引用本文:张晗宇,温维,程水源,吕喆.京津冀区域典型重污染过程与反馈效应研究[J].中国环境科学,2018,38(4):1209-1220.
作者姓名:张晗宇  温维  程水源  吕喆
作者单位:1. 北京工业大学, 区域大气复合污染防治北京市重点实验室, 北京 100124; 2. 中国气象局北京城市气象研究所, 北京 100089
基金项目:国家重点研发计划(2017YFC0209905);国家自然科学基金资助项目(51638001,91544232);北京市科学技术委员会(Z161100004516013,Z171100002217002);北京市自然科学基金资助项目(8172051)
摘    要:以京津冀地区2014年10月5~12日一次重污染过程为例,采用飞机AMDAR数据和WRF-Chem模式,分析了大气边界层垂直结构与PM2.5的时空演变规律,定量研究了气溶胶直接反馈效应对多种气象要素的影响.结果表明:此次重污染过程地域范围广、持续时间长、影响强度大,PM2.5污染呈带状分布,主要受地面均压场和高空纬向环流形成稳定的大气环流背景场、垂直层风场及逆温共同影响.气溶胶直接反馈效应导致京津冀地区整个时段太阳辐射量降低39.80W/m2,气温下降0.34℃,边界层高度降低36.64m,相对湿度升高0.90%.反馈效应南部地区较北部更显著,污染日强于平均时段和清洁天,气溶胶的辐射反馈作用使得各气象要素均呈现不利于污染物扩散的趋势,造成气溶胶聚集区PM2.5浓度进一步增加.

关 键 词:重污染  大气边界层  气溶胶直接反馈效应  WRF-Chem  
收稿时间:2017-09-02

Study on typical heavy pollution process and feedback effect in Beijing-Tianjin-Hebei region
ZHANG Han-yu,WEN Wei,CHENG Shui-yuan,LV Zhe.Study on typical heavy pollution process and feedback effect in Beijing-Tianjin-Hebei region[J].China Environmental Science,2018,38(4):1209-1220.
Authors:ZHANG Han-yu  WEN Wei  CHENG Shui-yuan  LV Zhe
Affiliation:1. Key Laboratory of Beijing on Regional Air Pollution Control, Beijing University of Technology, Beijing 100124, China; 2. Institute of Urban Meteorology, China Meteorological Administration, Beijing 100089, China
Abstract:Taking the heavy pollution episode in Beijing-Tianjin-Hebei region from October 5th to 12th, 2014 as an example, the aircraft AMDAR data and WRF-Chem model were applied to the evolution analysis of atmospheric boundary layer vertical structure and PM2.5 temporal and spatial characteristic. The aerosol direct feedback effect on multiple meteorological factors was simulated and quantitatively estimated. The results indicated that the heavy pollution process presented the characteristics including long duration, wide influencing region, large intensity and a tape-shape distribution of PM2.5 pollution, which was mainly affected by the uniform pressure field of ground, stable atmospheric background formed by latitudinal circulation in upper air, the vertical structure distribution of wind field and inversion structure. Aerosol direct feedback led to the following effect:(1) solar radiation reduced by 39.80W/m2; (2) temperature reduced by 0.34℃; (3) the boundary layer height reduced by 36.64m; (4) relative humidity increased by 0.90%. The feedback effect in the southern region was more obvious than that in the north region. The feedback effect in the pollution days was stronger than the average periods and clean days. The feedback effect makes the meteorological elements appear to be unfavorable to the diffusion of pollutants, and results in the further increase of PM2.5 concentration.
Keywords:heavy pollution  atmospheric boundary layer  aerosol direct feedback  WRF-Chem  
本文献已被 CNKI 等数据库收录!
点击此处可从《中国环境科学》浏览原始摘要信息
点击此处可从《中国环境科学》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司    京ICP备09084417号-23

京公网安备 11010802026262号