Measuring the Vertical Profiles of Aerosol Extinction in the Lower Troposphere by MAX-DOAS at a Rural Site in the North China Plain

被引:5
|
作者
Cheng, Siyang [1 ,2 ]
Jin, Junli [3 ]
Ma, Jianzhong [1 ,2 ]
Xu, Xiaobin [1 ,2 ]
Ran, Liang [4 ]
Ma, Zhiqiang [5 ]
Chen, Junming [1 ,2 ]
Guo, Junrang [1 ,2 ]
Yang, Peng [6 ]
Wang, Yang [7 ]
Wagner, Thomas [7 ]
机构
[1] Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China
[2] Chinese Acad Meteorol Sci, CMA Key Lab Atmospher Chem, Beijing 100081, Peoples R China
[3] CMA Meteorol Observat Ctr, Beijing 100081, Peoples R China
[4] Chinese Acad Sci, Key Lab Middle Atmosphere & Global Environm Obser, Inst Atmospher Phys, Beijing 100029, Peoples R China
[5] China Meteorol Adm, Inst Urban Meteorol, Beijing 100089, Peoples R China
[6] Meteorol Bur Shijiazhuang, Shijiazhuang 050081, Hebei, Peoples R China
[7] Max Planck Inst Chem, D-55020 Mainz, Germany
基金
中国国家自然科学基金;
关键词
aerosol extinction; vertical profile; ground-based MAX-DOAS; lidar; North China plain; OPTICAL-PROPERTIES; COLUMN DENSITIES; O-4; ABSORPTIONS; NO2; RETRIEVAL; SO2; WINTER; LIDAR; HCHO; VALIDATION;
D O I
10.3390/atmos11101037
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Ground-based multi-axis differential optical absorption spectroscopy (MAX-DOAS) measurements were performed during the summer (13 June-20 August) of 2014 at a rural site in North China Plain. The vertical profiles of aerosol extinction (AE) in the lower troposphere were retrieved to analyze the temporal variations of AE profiles, near-surface AE, and aerosol optical depth (AOD). The average AOD and near-surface AE over the period of study were 0.51 +/- 0.26 and 0.33 +/- 0.18 km(-1) during the effective observation period, respectively. High AE events and elevated AE layers were identified based on the time series of hourly AE profiles, near-surface AEs and AODs. It is found that in addition to the planetary boundary layer height (PBLH) and relative humidity (RH), the variations in the wind field have large impacts on the near-surface AE, AOD, and AE profile. Among 16 wind sectors, higher AOD or AE occur mostly in the directions of the cities upstream. The diurnal variations of the AE profiles, AODs and near-surface AEs are significant and influenced mainly by the source emissions, PBLH, and RH. The AE profile shape from MAX-DOAS measurement is generally in agreement with that from light detection and ranging (lidar) observations, although the AE absolute levels are different. Overall, ground-based MAX-DOAS can serve as a supplement to measure the AE vertical profiles in the lower troposphere.
引用
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页数:17
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