Lower tropospheric distributions of O3 and aerosol over Raoyang, a rural site in the North China Plain

被引:44
|
作者
Wang, Rui [1 ,2 ]
Xu, Xiaobin [1 ,2 ]
Jia, Shihui [1 ,2 ,7 ]
Ma, Ruisheng [3 ]
Ran, Liang [4 ]
Deng, Zhaoze [4 ]
Lin, Weili [5 ]
Wang, Ying [1 ,2 ]
Ma, Zhiqiang [6 ]
机构
[1] Chinese Acad Meteorol Sci, State Key Lab Severe Weather, China Meteorol Adm, Beijing, Peoples R China
[2] Chinese Acad Meteorol Sci, Key Lab Atmospher Chem, China Meteorol Adm, Beijing, Peoples R China
[3] Guangxi Meteorol Disaster Mitigat Inst, Nanning, Guangxi, Peoples R China
[4] Chinese Acad Sci, Inst Atmospher Phys, Key Lab Middle Atmosphere & Global Environm Obser, Beijing, Peoples R China
[5] China Meteorol Adm, Meteorol Observat Ctr, Beijing, Peoples R China
[6] China Meteorol Adm, Inst Urban Meteorol, Beijing, Peoples R China
[7] South China Univ Technol, Sch Environm & Energy, Guangzhou, Guangdong, Peoples R China
基金
中国国家自然科学基金;
关键词
PLANETARY BOUNDARY-LAYER; SURFACE OZONE; VERTICAL-DISTRIBUTION; SIGNIFICANT INCREASE; SULFATE AEROSOLS; LONG-TERM; CLIMATE; LIDAR; TRENDS; IMPACT;
D O I
10.5194/acp-17-3891-2017
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The North China Plain (NCP) has become one of the most polluted regions in China, with the rapidly increasing economic growth in the past decades. High concentrations of ambient O-3 and aerosol have been observed at urban as well as rural sites in the NCP. Most of the in situ observations of air pollutants have been conducted near the ground so that current knowledge about the vertical distributions of tropospheric O-3 and aerosol over the NCP region is still limited. In this study, vertical profiles of O-3 and size-resolved aerosol concentrations below 2.5 km were measured in summer 2014 over a rural site in the NCP, using an unmanned aerial vehicle (UAV) equipped with miniature analyzers. In addition, vertical profiles of aerosol scattering property in the lower troposphere and vertical profiles of O-3 below 1 km were also observed at the site using a lidar and tethered balloon, respectively. The depths of the mixed layer and residual layer were determined according to the vertical gradients of lidar particle extinction and aerosol number concentration. Average O-3 and size-resolved aerosol number concentration in both the mixed and residual layer were obtained from the data observed in seven UAV flights. The results show that during most of the flights the O-3 levels above the top of mixed layer were higher than those below. Such a positive gradient in the vertical distribution of O-3 makes the residual layer an important source of O-3 in the mixed layer, particularly during the morning when the top of mixed layer is rapidly elevated. In contrast to O3, aerosol number concentration was normally higher in the mixed layer than in the residual layer, particularly in the early morning. Aerosol particles were overwhelmingly distributed in the size range < 1 mu m, showing slight differences between the mixed and residual layers. Our measurements confirm that the lower troposphere over the rural area of the NCP is largely impacted by anthropogenic pollutants locally emitted or transported from urban areas. Compared with the historic O-3 vertical profiles over Beijing from the Measurement of Ozone and Water Vapor by Airbus In-Service Aircraft (MOZAIC), a strong increase in O-3 can be found at all heights below 2.5 km in the decade from 2004 to 2014, with the largest enhancement of about 41.6 ppb. This indicates that the lower troposphere over the northern part of the NCP has experienced rapidly worsening photochemical pollution. This worsening trend in photochemical pollution deserves more attention in the future.
引用
收藏
页码:3891 / 3903
页数:13
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