首页 | 本学科首页   官方微博 | 高级检索  
     检索      

广州地区旱季一次典型灰霾过程的特征及成因分析
引用本文:李菲,吴兑,谭浩波,毕雪岩,蒋德海,邓涛,陈欢欢,邓雪娇.广州地区旱季一次典型灰霾过程的特征及成因分析[J].热带气象学报,2012,28(1):113-122.
作者姓名:李菲  吴兑  谭浩波  毕雪岩  蒋德海  邓涛  陈欢欢  邓雪娇
作者单位:1. 北京大学物理学院大气与海洋科学系,北京100871;中国气象局广州热带海洋气象研究所,广东广州510080
2. 中国气象局广州热带海洋气象研究所,广东广州,510080
3. 汕头市气象局,广东汕头,515000
基金项目:863”课题(2006AA06A306、2006AA06A308);国家自然科学青年基金(40905018);广东省自然科学基金(033029); 《2010年第16届亚运会广州空气质量保障措施研究》项目共同资助
摘    要:通过研究2009年11月广州市气溶胶颗粒物质量浓度(PM10、PM2.5、PM1)、黑碳浓度、散射系数(Scatter)等大气成分要素,以及微波辐射计、激光雷达及风廓线雷达所探测的风、温、湿等边界层结构,统计分析广州旱季一次典型灰霾过程(2009年11月23—29日)中气溶胶颗粒物及其光学特性的时空变化特征,并配合天气形势背景、边界层结构对其形成原因进行详细分析。在典型灰霾过程中,黑碳浓度高达58.7μg/m3,散射系数高达1 902.7 Mm-1,PM10浓度高达423.5μg/m3,PM2.5浓度高达355.7μg/m3,PM1浓度高达286.5μg/m3。通过对同期的气象条件分析表明在广州地区旱季,区域性污染过程,特别是灰霾天气的形成具有以下三种气象条件:大气边界层高度较低;高压变性出海的天气形势与之密切相关;在偏东和偏南气流带来的高湿度环境下,气溶胶吸湿增长效应显著,导致出现严重灰霾天气。

关 键 词:典型灰霾过程  扩散条件  天气背景  广州地区  旱季
收稿时间:2011/3/25 0:00:00
修稿时间:2011/10/8 0:00:00

THE CHARACTERISTICS AND CAUSES ANALYSIS OF A TYPICAL HAZE PROCESS DURING THE DRY SEASON OVER GUANGZHOU AREA: A CASE STUDY
LI fei,WU dui,TAN Hao-bo,BI Xue-yan,JIANG De-hai,DENG tao,CHEN Huan-huan and DENG Xue-jiao.THE CHARACTERISTICS AND CAUSES ANALYSIS OF A TYPICAL HAZE PROCESS DURING THE DRY SEASON OVER GUANGZHOU AREA: A CASE STUDY[J].Journal of Tropical Meteorology,2012,28(1):113-122.
Authors:LI fei  WU dui  TAN Hao-bo  BI Xue-yan  JIANG De-hai  DENG tao  CHEN Huan-huan and DENG Xue-jiao
Institution:Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing 100871, China;Guangzhou Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080, China;Guangzhou Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080, China;Guangzhou Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080, China;Guangzhou Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080, China;Guangzhou Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080, China;Guangzhou Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080, China;Shantou Meteorological Bureau, Shantou 515000, China;Guangzhou Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080, China
Abstract:A study is made with the dataset(observed in November 2009,Guangzhou),which includes aerosol particle mass concentration(PM10,PM2.5,PM1),black carbon concentration,scattering coefficient,microwave radiometer measurements,laser radar and wind profiler data such as boundary layer structure of wind,temperature,and humidity.Statistical analyses are made for optical properties of aerosol particles and their spatial and temporal variations.With weather situation,meteorological background and boundary layer structure,a detailed analysis is presented of the causes of a typical haze process during the dry season(23—29 November 2009) over Guangzhou area.In the course of this typical haze,the concentration of black carbon was 58.7 μg/m3,scattering coefficient 1902.7 Mm-1,PM10 concentration 423.5 μg/m3,PM2.5 concentration 355.7 μg/m3,and PM1 concentration 286.5 μg/m3.Weather conditions over the same period showed that during the dry season over Guangzhou area,a process of regional pollution,especially the formation of a haze process,is accompanied with low atmospheric boundary layer and closely related with high variability of weather situation at sea.In the easterly and southerly flow of high humidity environment,significant aerosol hygroscopic growth results in severe haze.
Keywords:typical haze process  diffusion conditions  meteorological background  Guangzhou area  dry season
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《热带气象学报》浏览原始摘要信息
点击此处可从《热带气象学报》下载免费的PDF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