利用太阳光度计进行北京地区气溶胶光学性质研究

大气与环境光学学报 ›› 2018, Vol. 13 ›› Issue (2): 88-96.

利用太阳光度计进行北京地区气溶胶光学性质研究

牟福生1,3，李素文1，李昂3，谢品华2,3，王杨2，徐晋2，陈浩2，吴丰成2

（1 淮北师范大学物理与电子信息学院，安徽淮北 235000;
2 中国科学院安徽光学精密机械研究所中国科学院环境光学与技术重点实验室，安徽合肥 230031;
3 中国科学技术大学环境科学与光电技术学院，安徽合肥 230031）

收稿日期:2016-09-07 修回日期:2016-09-17 出版日期:2018-03-28 发布日期:2018-04-15
通讯作者: 牟福生(1987-)，男，山东烟台人，博士研究生，主要从事地基MAX-DOAS等遥感方面的研究。 E-mail:fsmou@aiofm.ac.cn
作者简介:牟福生(1987-)，男，山东烟台人，博士研究生，主要从事地基MAX-DOAS等遥感方面的研究。
基金资助:
Supported by National Natural Science Foundation of China(国家自然科学基金, 41705012, 41475017, 61275151, 91544104), National High Technology Research and Development Program(国家863计划, 2014AA06A511, 2014AA06A508), Anhui Natural Science Foundation(安徽省自然科学基金, 1308085QF124, 1508085QD71), Ahui University of Natural Science Foundation(安徽省高校自然科学基金, KJ2017B013, KJ2015A069)

Aerosol Optical Properties in Beijing Based on Observation by Sun-Photometer

MOU Fusheng1, LI Suwen1, LI Ang1, XIE Pinhua1,2, WANG Yang1, XU Jin1, CHEN Hao1, WU Fengcheng1

（1 College of Physics and Electronic Information, Huaibei Normal University, Huaibei 235000, China;
2 Key Laboratory of Environment Optics and Technology, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Science, Hefei 230031, China;
3 School of Environmental Science and Optoelectronic Technology, University of Science and Technology of China, Hefei 230031, China）

Received:2016-09-07 Revised:2016-09-17 Published:2018-03-28 Online:2018-04-15
Supported by:
Supported by National Natural Science Foundation of China(国家自然科学基金, 41705012, 41475017, 61275151, 91544104), National High Technology Research and Development Program(国家863计划, 2014AA06A511, 2014AA06A508), Anhui Natural Science Foundation(安徽省自然科学基金, 1308085QF124, 1508085QD71), Ahui University of Natural Science Foundation(安徽省高校自然科学基金, KJ2017B013, KJ2015A069)

摘要/Abstract

摘要：

利用2011年到2014年北京太阳光度计数据对北京地区的气溶胶光学特性进行了研究。北京地区气溶胶光学厚度（AOD）全年较高，四年440nm波长的AOD年均值分别是0.67±0.70，0.69±0.71，0.73±0.66，0.75±0.66。AOD月均值表现出一定的季节变化，最大值和最小值一般出现在春季和秋季。通过气溶胶类型分类可知，除了春季受沙尘大颗粒气溶胶影响外，北京地区高气溶胶主要是由城市细粒子气溶胶引起，且四季小粒子增长现象明显，其中夏秋季主要为吸湿性增长，其他季节主要为静稳天气下的增长。通过对比沙尘和霾天气下气溶胶性质进行对比，结果表明:霾天气下AOD一般高于沙尘天气。Hysplit风场后向轨迹模型结果表明，沙尘天气下气团为穿过蒙古草原和沙漠的西北风场。在灰霾天气下风场风速较小且主要以东南和西南风场为主，高气溶胶状态为本地积累和外来输送共同作用产生。

关键词: 气溶胶光学特性, 气溶胶分类, 太阳光度计

Abstract:

Aerosol optical properties are studied using the data from 2011 to 2014 at Beijing station. It shows the aerosol optical depth in Beijing is high for the whole year, the annual mean of aerosol optical depth (AOD) at 440 nm for the four years are about 0.67±0.70，0.69±0.71，0.73±0.66 and 0.75±0.66, respectively. The average monthly AOD shows similar seasonal variation with a maximum in spring and a minimum in autumn. According to aerosol classification high aerosol level in Beijing is mainly caused by fine particles and there are also coarse dust particles in spring. Fine particles growth is found in four seasons , which is mainly a hygroscopic growth in summer and autumn and a coagulation growth in other seasons. Comparison of aerosol properties between dust and haze condition shows AOD in haze condition is general higher than that in dust condition and AOD at 440nm is 3.7 times than that in dust condition. The back trajectory analysis indicates that air-masses on the dust day are northwest wind across Mongolia grassland and Gobi deserts. The wind speed on the haze day is weak and dominated by southeast and northwest wind, and high aerosol load condition is caused by local accumulation and transportation from other places.

Key words: aerosol optical properties, aerosol classification, sun-photometer

中图分类号:

X513

牟福生李素文李昂谢品华王杨徐晋陈浩吴丰成. 利用太阳光度计进行北京地区气溶胶光学性质研究[J]. 大气与环境光学学报, 2018, 13(2): 88-96.

MOU Fu-Sheng, LI Su-Wen, LI Ang, XIE Pin-Hua, WANG Yang, XU Jin, CHEN Hao, WU Feng-Cheng. Aerosol Optical Properties in Beijing Based on Observation by Sun-Photometer[J]. Journal of Atmospheric and Environmental Optics, 2018, 13(2): 88-96.

参考文献

[1]Zhang Chengchang, Zhou Wenxian. Atmospheric Aerosol Tutorial [M]. Beijing: China Meteorological Press, 1995: 299-323(in Chinese).
章澄昌, 周文贤. 大气气溶胶教程 [M].气象出版社, 1995: 299-323.
[2] Biggar S F, Gellman D I, Slater P N. Improved evaluation of optical depth components from Langley plot data [J]. Remote Sens. Environ., 1990, 32: 91-101.
[3] Rosenfeld D. Aerosols, clouds, and climate [J].Science, 2006, 312(5778): 1323-1324.
[4] Qiu Jinhuan, Lv Daren, Chen Hongbin, et al. Modern research progress in atmospheric physics [J]. Chinese Journal of Atmospheric Science, 2003, 27(4): 628-652(in Chinese).
邱金桓, 吕达仁, 陈洪滨, 等. 现代大气物理学研究进展 [J]. 大气科学, 2003, 27(4): 628-652.
[5] Holben B N, Eck T F, Slutsker I, et al. AERONET-A federated instrument network and data achieve for aerosol characterization [J]. Rem. Sens. Environ., 1998, 66(1): 1-16.
[6] Che H Z, Shi G, Uchiyama A, et al. Intercomparison between aerosol optical properties by a PREDE skyradiometer and CIMEL sunphotometer over Beijing, China [J]. Atmos. Chim. Phys., 2008, 8: 3199-3214.
[7] Zhao H, Che H, Zhang X, et al. Aerosol optical properties over urban and industrial region of Northeast China by using ground-based sun-photometer measurement [J]. Atmos. Environ., 2013, 75: 270-278.
[8] Pan L, Che H Z, Geng F H, et al. Aerosol optical properties based on ground measurements over the Chinese Yangtze Delta Region [J]. Atmos. Environ., 2010, 44: 2587-2596.
[9] Fan X H, Chen H B, Goloub P, et al. Analysis of column-integrated aerosol optical thickness in Beijing from AERONET observation [J]. China Particuology, 2006, 4(6): 300-335.
[10] Wang P, Che H Z, Zhang X Y, et al. Aerosol optical properties of regional background atmosphere in Northeast China [J]. Atmos. Environ., 2010, 44: 4404-4412.
[11] Che H Z, Yang Z F, Zhang X, et al. Study on the aerosol optical properties and their relationship with aerosol chemical compositions over three regional background stations in China [J]. Atmos. Environ., 2009, 43(5): 1093-1099.
[12] Ren Yiyong, Li Xia, Lv Ming. Application prospect of measurement by sun photometer CE318 and retrieval methodology [J]. Meteorological Science and Technology, 2006, 34(3): 349-352(in Chinese)
任宜勇, 李霞, 吕鸣, 等. CE318太阳光度计观测资料应用前景及其解读 [J]. 气象科技, 2006, 34(3): 349-352.
[13] Che H, Zhang X, Alfraro S, et al. Aerosol optical properties and its radiative forcing over Yulin, China in 2001 and 2002 [J].Adv. Atmos. Sci., 2009, 26(3): 564-576.
[14] Xia X A, Chen H B, Wang P C, et al. Aerosol properties and their spatial and temporal variations over north China in spring 2001 [J]. Tellus B, 2005, 57(1): 28-39.
[15] Cheng Nianliang, Li Yunting, Zhang Dawei. Analysis about the characteristics and formation mechanisms of serious pollution events in October 2014, in Beijing [J]. Research of Environmental Sciences, 2015, 28(2): 163-170(in Chinese)．
程念亮, 李云婷, 张大伟. 2014 年 10 月北京市4次典型空气重污染过程成因分析 [J]. 环境科学研究, 2015, 28(2): 163-170．
[16] Li Bengang, Ran Yang, Tao Peng. Season variation and spatial distribution of atmospheric aerosols in Beijing [J]. Acta Scientiae Circumstantiae, 2008, 28(7): 1425-1429(in Chinese).
李本纲, 冉阳, 陶澍. 北京市气溶胶的时间变化与空间分布特征 [J]. 环境科学学报, 2008, 28(7): 1425-1429.
[17] Gobbi G P, Kaufman Y J, Koren I, et al. Classification of aerosol properties derived from AERONET direct sun data [J]. Atmos. Chem. Phys., 2007, 7(2): 453-458.
[18] Liu Ruiting, Han Zhiwei, Li Jiawei. Analysis of meteorological characteristics during winter haze events in Beijing [J]. Climatic and Environmental Research, 2014, 19(2): 164-172(in Chinese). 刘瑞婷, 韩志伟, 李嘉伟. 北京冬季雾霾事件的气象特征分析 [J]. 气候与环境研究, 2014, 19(2): 164-172.
[19] Brimelow J C, Reuter G W. Transport of atmospheric moisture during three extreme rainfall events over the Mackenzie River basin [J]. J. Hydrometeorol., 2005, 6(4): 423-440.
[20] Zhang R, Fu C, Han Z, et al. Characteristics of elemental composition of PM2.5 in the spring period at Tongyu in the semi-arid region of Northeast China [J]. Adv. Atmos. Sci., 2008, 25(6): 922-931.