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天津城市大气污染物浓度垂直分布特征
引用本文:黄鹤,孙玫玲,刘爱霞,张长春.天津城市大气污染物浓度垂直分布特征[J].环境科学学报,2009,29(12):2478-2483.
作者姓名:黄鹤  孙玫玲  刘爱霞  张长春
作者单位:1. 中国气象局北京城市气象研究所,北京,100089;天津市气象科学研究所,天津,300061
2. 天津市气象科学研究所,天津,300061
基金项目:2008年度城市气象科学研究基金(No.UMRF200806);天津市自然科学基金(No. 08GCYBGC10200);天津市气象局研究型业务基金(No. YJX0808)
摘    要:利用2007年10月10日~2008年9月30日天津边界层气象观测塔得到的PM2.5质量浓度、O3和NO2体积分数等梯度资料,对比分析了不同高度上各污染物数据统计特征,并对各污染物数据的时间变化特征及垂直分布进行了讨论.结果表明,天津市PM2.5污染严重,且易发生光化学污染事件.各高度层PM2.5浓度在12、1和2月份存在较大差异,其他月份差异较小;O3体积分数均表现出夏季高冬季低的典型特征;NO2体积分数在220m高度处变化较为复杂且全年波动较大,120m处变化平稳,40m处则表现出春夏季高、秋冬季低的特点.PM2.5体积分数和NO2体积分数日变化均呈现双峰型,峰值的出现与早晚出行高峰以及边界层的变化有关,且污染物出现峰值的时间由低到高存在2~3h的延迟.O3体积分数与太阳辐射强度关系密切,各层均在14:00前后达到最大,而夜间的还原反应使各层臭氧体积分数下降.40m和120m处NO2体积分数变化较为一致,全天波动很小,而220m处波动较大,昼夜差异明显.

关 键 词:边界层  污染物浓度  统计特征  时间变化  垂直分布
收稿时间:2/7/2009 1:00:34 PM
修稿时间:8/27/2009 9:16:44 AM

Vertical distribution of air pollutants in the atmosphere in Tianjin
HUANG He,SUN Meiling,LIU Aixia and ZHANG Changchun.Vertical distribution of air pollutants in the atmosphere in Tianjin[J].Acta Scientiae Circumstantiae,2009,29(12):2478-2483.
Authors:HUANG He  SUN Meiling  LIU Aixia and ZHANG Changchun
Institution:1. Institute of Urban Meteorology, CMA, Beijing 100089; 2. Tianjin Meteorology Institute, Tianjin 300061,Tianjin Meteorology Institute, Tianjin 300061,Tianjin Meteorology Institute, Tianjin 300061 and Tianjin Meteorology Institute, Tianjin 300061
Abstract:The statistical characteristics, temporal variation and vertical distribution of the main air pollutants in Tianjin (PM_(2.5), O_3 and NO_2 ) were analyzed using the vertical data obtained from a 255 m meteorological tower from 10, Oct 2007 to 30, Sept 2008. In Tianjin, the major pollutant is PM_(2.5), and photochemical smog easily occurs due to the high O_3 concentration. The differences of PM_(2.5) concentration among the three heights (220m,120m and 40m) are greater in December, January and February than in other months. All the O_3 concentrations in the three layers are larger in summer,but smaller in winter. The NO_2 concentration fluctuates obviously at 220m, but is relatively stable at 120m and at 40m. The NO_2 concentration is greater in spring and summer than in autumn and winter. The daily PM_(2.5) and NO_2 concentrations both have two peaks at the morning and evening rush hours and the boundary layer moves. According to the times of appearance of each peak at each layer, 2-3 hours are required to transfer the pollutants from the ground to the top layer. The O_3 concentration has a close relationship with the solar radiation intensity and reaches to a maximum at about 14:00 and decreases at night because of the deoxidization reactions in each atmospheric layer. Both at 40 m and 120 m, the concentration of NO_2changes similarly and oscillates little, but at 220 m it fluctuates obviously, and in addition, shows a greater diurnal variation.
Keywords:boundary layer  pollution concentration  statistical characteristics  temporal variation  vertical distribution
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