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利用WRF-Chem模拟研究京津冀地区夏季大气污染物的分布和演变
引用本文:庞杨,韩志伟,朱彬,李嘉伟.利用WRF-Chem模拟研究京津冀地区夏季大气污染物的分布和演变[J].南京气象学院学报,2013(6):674-682.
作者姓名:庞杨  韩志伟  朱彬  李嘉伟
作者单位:[1]南京信息工程大学大气物理学院,江苏南京210044 [2]中国科学院东亚区域气候-环境重点实验室,北京100029
摘    要:应用WRF—Chem(Weather Research and Forecasting Model with Chemistry)模式模拟研究了2007年8月京津冀地区近地面O3、NO2、PM2.5浓度的时空变化特征,将模拟结果与观测数据进行详细对比,结果表明,模式可以较好地模拟O3、PM2.5,浓度的空间分布和时间变化特征,成功再现了8月33和PM2.5的几次积累增加过程,其中O,的模拟值与观测值的相关系数为0.69~0.86,PM2.5的相关系数为0.44~0.49,但模式对NO2的模拟相对较差,相关系数为0.27~0.43。北京、天津地区为O3月均低值区,月均体积浓度约30×10^-9,渤海及京津冀以西地区O3月平均体积浓度可达60×10^-9;PM2,呈现南高北低的分布特征,变化范围为120~240μg/m3。14时月平均03体积浓度在北京、天津地区低于周边地区,约为60×10^-9;而PM2.5质量浓度在环渤海地区和河北南部较高,为100~120μg/m^3。8月17日北京出现一次典型的高浓度O,污染事件,14时北京地区温度达到33℃,O3体积浓度为80×10^-9~110×10^-9。在局地排放、化学反应和外来输送的共同作用下,渤海西岸和北岸PM2.5的质量浓度超过120μg/m3,其中二次气溶胶质量浓度为50~100μg/m3,一次排放人为气溶胶质量浓度为10~20μg/m3,海盐质量浓度为1~7μg/m3,二次气溶胶是该地区PM2.5的主要贡献者。

关 键 词:O3  NO2  PM2  5  污染物分布和演变  数值模拟

A model study on distribution and evolution of atmospheric pollutants over Beijing-Tianjin-Hebei region in summertime with WRF-Chem
PANG Yang,HAN Zhi-wei,ZHU Bin,LI Jia-wei.A model study on distribution and evolution of atmospheric pollutants over Beijing-Tianjin-Hebei region in summertime with WRF-Chem[J].Journal of Nanjing Institute of Meteorology,2013(6):674-682.
Authors:PANG Yang  HAN Zhi-wei  ZHU Bin  LI Jia-wei
Institution:2 ( 1. School of Atmospheric Physics, NUIST, Nanjing 210044, China; 2. Key Laboratory of Regional Climate-Environment for East Asia (RCE-TEA), Chinese Academy of Sciences, B eijing 100029, China)
Abstract:In this paper, the WRF-Chem model was used to analyze the temporal and spatial variations of the near-surface concentrations of ozone ( 03 ), nitrogen dioxide ( NO2 ) and fine particulate matter (PM2.5 ) over the Beijing-Tianjin-Hebei region in August 2007. The simulation results were compared with surface observations. It was indicated that the model could reproduce the temporal and spatial vari- ations of 03 and PM2. 5 reasonably well and successfully reflect several pollution events in August 2007. However, the model' s performance was relatively poor for NO2. The correlation coefficients between the model simulations and the observations were 0. 69-0. 86 for 03 ,0.440. 49 for PM2.5 and 0.27- 0. 43 for NO2. In August, the monthly mean concentration of O3 in Beijing and Tianjin was relatively low at about 30 x 10 -9 whereas relatively high P3 concentration ( about 60 x 10 -9 ) was predicted in the west of the Beijing-Tianjin-Hebei region and over the Bohai Bay. The PM2. 5 showed higher concentra- tion levels in the south than in the north within the Beijing-Tianjin-Hebei region with the monthly mean concentrations ranging from 120 to 240μg/m3. The monthly mean 03 concentration at 14:00 BST in August was about 60 x 10-9 in Beijing and Tianjin, which was lower than those in the surrounding are- as. The mean PM2.5 concentrations at 14:00 BST showed higher levels( 100-120 μg/m3) in the south- ern parts of the Hebei province and the Bohai Bay areas. An O3 pollution episode occurred on August 17 when the air temperature in Beijing reached 33 ℃ at 14:00 BST,resulting in high concentration of 03 (80 ×10-9-110 × 10-9). Meanwhile ,due to the combined effects of local emission, chemical reac- tion and trans-boundary transport, the PM2.5 concentration in the west and the north of the Bohai bay was as high as over 120 μg/m3 ,in which the secondary aerosols formed through chemical reactions, the primary anthropogenic aerosols released directly and sea salt aerosols accounted for about 50-100μg/m3, 10--20 μg/m3 and 1--7 μg/m3 ,respectively. Thus, the secondary aerosols were the main con- tributor to PM2. 5 in these areas during this episode.
Keywords:O3  NO2  PM2  5  pollutant distribution and evolution  numerical simulation
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