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大气传输对华北区域本底地区降水化学成分的影响
引用本文:徐敬,张小玲,徐晓斌,于晓岚,程红兵,周怀刚.大气传输对华北区域本底地区降水化学成分的影响[J].气候与环境研究,2011,16(1):105-112.
作者姓名:徐敬  张小玲  徐晓斌  于晓岚  程红兵  周怀刚
作者单位:1. 中国气象局北京城市气象研究所,北京100089;中国气象科学研究院,北京,100081;中国科学院研究生院,北京100049
2. 中国气象局北京城市气象研究所,北京100089;北京上甸子大气成分本底国家野外站,北京101507
3. 中国气象科学研究院,北京,100081
4. 北京上甸子大气成分本底国家野外站,北京,101507
基金项目:中国气象局公益性行业(气象)科研专项GYHY20080602
摘    要:对华北区域本底站1999~2007年239次降水过程的气流后向轨迹进行分类,从中选取典型西北路径、西南路径和东南路径降水,研究了不同输送路径下降水pH值、电导率、化学组成特征及影响本底地区的主要排放源.结果显示,起源于我国中东部内陆地区途经太原、石家庄、北京等大城市的西南气流,起源于蒙古国途经我国内蒙地区的西北气流,以...

关 键 词:传输  本底  降水化学

Influence of Atmospheric Transportation on Chemical Compositions of Precipitation in North China Regional Background Area
XU Jing,ZHANG Xiaoling,XU Xiaobin,YU Xiaolan,CHENG Hongbing and ZHOU Huaigang.Influence of Atmospheric Transportation on Chemical Compositions of Precipitation in North China Regional Background Area[J].Climatic and Environmental Research,2011,16(1):105-112.
Authors:XU Jing  ZHANG Xiaoling  XU Xiaobin  YU Xiaolan  CHENG Hongbing and ZHOU Huaigang
Institution:XU Jing 1,2,3,ZHANG Xiaoling1,4,XU Xiaobin2,YU Xiaolan2,CHENG Hongbing2,and ZHOU Huaigang41 The Institute of Urban Meteorology,China Meteorological Administration,Beijing 1000892 Chinese Academy of Meteorological Sciences,Beijing 100081 3 Graduate University of Chinese Academy of Sciences,Beijing 1000494 Shangdianzi National Station for Atmospheric Background Observation,Beijing 101507
Abstract:The backward trajectories of 239 precipitation processes from 1999 to 2007 at North China regional atmospheric background station were classified. Typical north-west, south-west and south-east backward trajectory precipitation samples were selected to research the characters of the precipitation pH, electrical conductivity, chemical composition, and the main sources affect the background area. Results showed that the south-west backward trajectory coming from the east-central inland area of China, passing through Taiyuan, Shijiazhuang, and Beijing, the north-west trajectory coming from Mongolia, passing through inner Mongolia area, and the south-east trajectory coming from oceanic area, passing through east coastal cities were the main backward trajectories affecting the precipitation at Shangdianzi station. The precipitation frequency in the south-west trajectory was the highest. The pH peaked in the south-west transportation direction and reached a minimum in the south-east. The electrical conductivities reached a maximum in the south-west transportation direction and a minimum in the north-west. SO2-4, NO-3, NH+4, and Ca2+ were the major ions of precipitation at Shangdianzi. The concentrations of the major ions of the south-west trajectory samples were much higher than that of the other directions. Soil dust, farm emission related to fertilization, pollutants from traffic and coal combustion emission were the main four sources identified affecting the background area. The natural source was the primary source affecting the background area in the north-west clean transportation direction, while the anthropogenic sources were more notable in the south-west transportation direction, such as traffic and coal combustion emission. Compare to 1999-2004, the averaged pH decreased from 2005 to 2007, which attributes to the decreasing of the concentrations of alkaline ions in precipitation. The results show that rainfall is significant for the conductivity, acid rain frequency, and the components of the precipitation. The values of conductivity and components concentration decrease and the acid rain frequency increase as the rainfall increase gradually.
Keywords:transportation  background  precipitation chemistry
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