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杭州市臭氧污染特征及影响因素分析
引用本文:严仁嫦,叶辉,林旭,何曦,陈超,沈建东,许凯儿,郑仙珏,王丽吉. 杭州市臭氧污染特征及影响因素分析[J]. 环境科学学报, 2018, 38(3): 1128-1136
作者姓名:严仁嫦  叶辉  林旭  何曦  陈超  沈建东  许凯儿  郑仙珏  王丽吉
作者单位:杭州市环境监测中心站, 杭州 310007,杭州市环境监测中心站, 杭州 310007,杭州市环境监测中心站, 杭州 310007,杭州市环境监测中心站, 杭州 310007,杭州市环境监测中心站, 杭州 310007,杭州市环境监测中心站, 杭州 310007,杭州市环境监测中心站, 杭州 310007,杭州市环境监测中心站, 杭州 310007,浙江省气象信息网络中心, 杭州 310017
基金项目:杭州市农业科研自主申报项目(No.20170533B15,20160533B83);2017年农业与社会发展主动设计项目(No.20172016A107)
摘    要:为研究杭州市夏季臭氧(O_3)污染特征及其影响因素,统计分析了2013—2016年杭州市O_3监测数据与杭州市气象数据,并结合AIRS卫星O_3数据探讨了台风天气系统对杭州市近地面O_3浓度的影响.结果表明:2013—2016年,杭州市O_3污染逐年加重,O_3浓度高值持续时间延长.O_3浓度与太阳辐射、温度相关,每年5月和8月太阳辐射强、温度高,O_3污染最严重;全天O_3浓度呈单峰日变化,峰值出现在午后(~14:00)太阳辐射较强、温度最高时.杭州市在日降水为0且12:00—15:00太阳辐射通量均值高于200 W·m~(-2)天气条件下,风向为东、东北或东南风且风速低于3 m·s~(-1)时,O_3浓度相对较高,易出现超标情况.台风天气系统对杭州市近地面O_3浓度有明显影响,以2014年10号台风"麦德姆"为例,台风外围系统影响到杭州时,偏东气流可将杭州以东地区高浓度O_3输送到杭州,同时下沉气流导致污染物在近地层积聚不易扩散,造成近地层O_3浓度升高.

关 键 词:O3  污染特征  气象要素  台风天气系统
收稿时间:2017-07-06
修稿时间:2017-10-09

Characteristics and influence factors of ozone pollution in Hangzhou
YAN Renchang,YE Hui,LIN Xu,HE Xi,CHEN Chao,SHEN Jiandong,XU Kaier,ZHENG Xianjue and WANG Liji. Characteristics and influence factors of ozone pollution in Hangzhou[J]. Acta Scientiae Circumstantiae, 2018, 38(3): 1128-1136
Authors:YAN Renchang  YE Hui  LIN Xu  HE Xi  CHEN Chao  SHEN Jiandong  XU Kaier  ZHENG Xianjue  WANG Liji
Affiliation:Hangzhou Environmental Monitoring Central Station, Hangzhou 310007,Hangzhou Environmental Monitoring Central Station, Hangzhou 310007,Hangzhou Environmental Monitoring Central Station, Hangzhou 310007,Hangzhou Environmental Monitoring Central Station, Hangzhou 310007,Hangzhou Environmental Monitoring Central Station, Hangzhou 310007,Hangzhou Environmental Monitoring Central Station, Hangzhou 310007,Hangzhou Environmental Monitoring Central Station, Hangzhou 310007,Hangzhou Environmental Monitoring Central Station, Hangzhou 310007 and Zhejiang Meteorological Information and Network Center, Hangzhou 310017
Abstract:To investigate the characteristics and essential influence factors of near-surface layer ozone (O3) pollution in Hangzhou, this article analyzed the national environmental monitoring O3 data and meteorological data of Hangzhou during 2013-2016. The O3 data derived from the Aqua Atmospheric Infrared Sounder (AIRS) were used to analyze the impact of typhoon system on surface O3 concentration in Hangzhou. The observational analysis shows that the O3 pollution became increasingly serious from 2013 to 2016 with extended duration of high-level O3. The O3 concentration showed obvious positive correlation with solar radiation and temperature. Severe high O3 episodes usually occurred in May and August because of strong solar radiation and high temperature. The diurnal variation of O3 concentration showed a unimodal distribution with a maximum in the afternoon (~14:00), corresponding to the strongest solar radiation and maximum temperature. The abnormally high O3 concentration was prone to occur when the following three conditions apply simultaneously:daily precipitation amounts is zero; the average solar radiation from 12:00 to 15:00 is higher than 200 W·m-2; easterly, northeast or southeast with wind speed lower than 3 m·s-1. In addition, the typhoon system has a significant effect on near-surface O3 concentration in Hangzhou. Taking typhoon Matmo in 2014 as an example, the surface O3 concentration in Hangzhou has remarkably increased due to the airflow of the typhoon periphery:the east airflow can transport the comparatively high concentration O3 from east region to Hangzhou, while the downward airflows lead to the accumulation of pollutants in the boundary layer.
Keywords:O3  pollution characteristics  meteorological factors  typhoon system
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