Abstract
The temporal and spatial distribution and variation characteristics of ozone (O3) in Beijing, China, are investigated using hourly monitoring data from 2020. Kriging interpolation analysis and correlation analysis are applied to describe the spatial-temporal distribution and to identify associated influencing factors. The average concentration of O3 was found to be 59.58 μg·m−3. The daily maximum sliding 8 h average ozone concentration values exceeded the primary standard (100 μg·m−3) for 129 days and exceeded the secondary standard (160 μg·m−3) for 48 days. Temporally, the general pattern of daily maximum 8 h average O3 concentration was high in spring and summer and low in autumn and winter. Monthly average values showed a maximum in June. The highest daily concentrations appeared between 13:00 and 18:00 local time, and O3 concentrations had a distinct weekly pattern of variability with daily average concentrations at weekends higher than those during working days. Spatially, annual average O3 concentrations were highest in the northeast and lowest in the southeast of the city, and the seasonal variation of O3 was most significant in the southwest of the city. In relation to city districts and counties, the annual average O3 concentrations in the Miyun District were the highest, while those in the Haidian District were the lowest. On the whole, annual average O3 concentrations in Beijing were higher in the suburbs than in central areas. Based on daily average values, there was no significant correlation between O3 concentrations and rainfall (p > 0.05), but there were significant correlations between O3 concentration and sunshine hours, wind speed, maximum temperature and minimum temperature (p < 0.05), with correlation coefficients of 0.158, 0.267, 0.724 and 0.703, respectively. O3 concentrations increased with an increasing number of sunshine hours, first increased and then decreased with increasing wind speed and increased with increasing temperature. O3 concentrations were correlated with SO2 concentrations (0.05 < p > 0.001), CO concentrations (p < 0.001) and NO2 concentrations (p < 0.001), the latter having the highest correlation coefficient of −0.553 and exhibiting opposite trends in daily and monthly variations to O3 variations. Analysis of ozone pollution sources showed that automobile exhaust, coal and oil combustion and volatile organic compounds released by industrial plants were the main sources. Terrain affected the distribution of ozone, as well as human activities and industry.
Highlights
Ozone (O3) is an important component of the atmosphere, most of which lies in the stratosphere, and a small part exists in the troposphere
O3 can absorb solar radiation reflected from the ground and re-emit the radiation, contributing to global warming and climatic change [1]
The increase of O3 concentrations in the troposphere can potentially affect the health of human beings, animals and plants
Summary
Ozone (O3) is an important component of the atmosphere, most of which lies in the stratosphere, and a small part exists in the troposphere. Stratospheric O3 can protect terrestrial organisms from radiation hazards by absorbing external ultraviolet radiation. O3 can absorb solar radiation reflected from the ground and re-emit the radiation, contributing to global warming and climatic change [1]. The precursors of tropospheric O3 are generally nitrogen oxides (NOx) and volatile organic compounds (VOCs) [2]. The reaction process is as follows: CO VOCs. The increase of O3 concentrations in the troposphere can potentially affect the health of human beings, animals and plants. In a high-concentration O3 environment, human beings are prone to respiratory diseases and the growth and output of crops are inhibited [4]. High O3 concentrations can cause agricultural and forestry industries to reduce their production and reduce their economic outputs
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