气象因子和海风对秦皇岛市臭氧污染的影响

doi:10.3969/j.issn.1673-503X.2021.02.009

Abstract

Abstract:

Based on the data of air pollution concentration from Qinhuangdao environmental monitoring station, the meteorological data from Qinhuangdao meteorological observation station and buoy station, the characteristics of O₃ pollution and its response to meteorological factors and the sea breeze were researched.Results show that the monthly variation of O₃ pollution in Qinhuangdao is characterized by the most serious in May-June and September, and no day with O₃ exceeding the standard in October-December and January-February.The diurnal variation of O₃ is unimodal distribution i.e.the O₃ concentration is highest in the afternoon and lowest in the morning.In general, the key meteorological factors triggering O₃ pollution in Qinhuangdao are solar radiation of 850-950 W·m^-2, daily maximum temperature over 32 ℃, relative humidity of 50%-60%, no precipitation, and SW or SSW wind dominant respectively.The sea breeze in Qinhuangdao is the most common phenomenon from June to August, with a frequency of over 50%.Usually, the sea breeze starts to appear at 8-10 a.m., reaches its maximum at noon-3 p.m., and weakens and is over after the evening.The average concentrations of O₃-8h on days with the sea breeze from May to June and August to September are higher than those on days without sea breeze, and the monthly average concentrations of O₃-8h on days with the sea breeze in May, June, and September are as high as 155-166 μg·m^-3.All these indicate that the circulation of sea-land breeze plays a role in aggravating O₃ pollution in Qinhuangdao.

Key words: Ozone, Meteorological factor, Sea breeze

CLC Number:

X515

Shi-ru ZHOU,Jin-mei SONG,Qian LU,Hong-ming GUO,Yu-guang ZHAO,Yan-chun GAO. The influences of meteorological factors and sea breeze on ozone pollution in Qinhuangdao[J]. Journal of Meteorology and Environment, 2021, 37(2): 64-70.

Figures/Tables 10

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The influences of meteorological factors and sea breeze on ozone pollution in Qinhuangdao

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