Characterizing the near-surface vertical variations of summertime O3 in Jiaxing
HE Guo-wen1, WU Dui1,2, WU Cheng1, LI Mei1, DENG Tao2, WU Wei-chao3, LI Li3, CHENG Peng1, YUAN Qian3, ZHANG Ying-long3, SONG Lang1, SUN Jia-yin1, TAO Li-ping1, LIANG Yue1, TAN Jian1, ZHOU Zhen1
1. Guangdong Engineering Research Centre for Online Atmospheric Pollution Source Appointment Mass Spectrometry System, Institute of Mass Spectrometry and Atmospheric Environment, Jinan University, Guangzhou 510632, China; 2. Institute of Tropical and Marine Meteorology, China Meteorological Administration, Guangzhou 510640; 3. Jiaxing Environmental Monitoring Station, Jiaxing 314000, China
Abstract:Based on O3 surface data in 2018 from 14 monitor stations and meteorological factors of Jiaxing city, Zhejiang Province, this study analyzed the relationship between O3 and meteorological factors. The vertical profile of O3 was characterized by a differential absorption O3 lidar. Temperature and relative humidity were the dominating factors for high concentration O3 pollution, with the range of 24~36℃ and 36%~77%, respectively. The temperature above 24℃ and the relative humidity below 77% can be used as the meteorological threshold for early warning of O3 pollution. The O3 lidar results showed that the vertical O3profiles were similar between episodic and clean days, which exhibited an O3 peak between 600~800m, while the O3 concentrations decreased beyond this range. During the O3 episodic period, O3 was transported downward to the ground~level from noon to afternoon. This superposition of near-surface ozone and ground-level ozone aggravates ground-level O3 pollution, leading to an exceedance of air quality standard for O3 at both near-surface and ground-level. The O3 below 800m was relatively constant at night and in the early morning. Ground-level O3 increased rapidly after sunrise until reaching a peak in the afternoon. O3 decreased gradually in the later afternoon. The backward trajectories clustering analysis showed that there was a similarity in the clusters of air masses at 10m, 500m, and 1000m. Air masses that traveled along the coastline of Fujian and Zhejiang provinces at 500m exhibited higher O3 than the air masses from the ocean at 10m. That was related to the transport accumulation of the precursors and the stronger ultraviolet radiation at 500m. During the episodic events, the near-surface air masses exhibited an unchanged height. The downdraft in the middle and upper boundary layer led to the accumulation of O3 precursor near 500m. That was one of the reasons for the high O3 near 500m observed in two typical pollution episodes.
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