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基于光学厚度光谱特征改进北京地区气溶胶积聚模态比例估计
引用本文:张莹,李正强,王堰,李凯涛,李东辉,张玉环,魏鹏,王玲,吕阳. 基于光学厚度光谱特征改进北京地区气溶胶积聚模态比例估计[J]. 光谱学与光谱分析, 2013, 33(10): 2795-2802. DOI: 10.3964/j.issn.1000-0593(2013)10-2795-08
作者姓名:张莹  李正强  王堰  李凯涛  李东辉  张玉环  魏鹏  王玲  吕阳
作者单位:1. 中国科学院遥感与数字地球研究所,北京 100101
2. 中国科学院大学,北京 100049
基金项目:国家重点基础研究发展规划项目,国家自然科学基金项目
摘    要:积聚模态比例(AMF)是细模态气溶胶光学厚度占总光学厚度的比例,是估算直接辐射强迫和评估细颗粒物污染的重要参数。利用2011年北京地区AERONET网站提供的气溶胶光学厚度(AOD)和粒子体积谱分布等微观参数,计算极值修正后的细模态Angstrom指数(αf)并进行气溶胶光学厚度光谱退卷积计算,改进AMF估算精度。AMF估算误差主要是由于αf的误差估计偏小造成的。通过统计模拟的αf极大值与极小值范围获取约束条件,建立极值修正方法。通过敏感性试验可知,极值修正可将αf约束在合理范围内,且αf和AMF对气溶胶归一化体积谱分布敏感,不同谱分布可使αf从0.662变化到2.849,AMF从0.08变化到0.84。经过极值修正后,AMF的平均误差从0.072减小到0.044,减小了38.89%,尤其在冬夏两季,误差减小明显。AMF精度的提高可直接提高细模态及人为气溶胶光学厚度的估算精度,对人为气溶胶的直接辐射强迫估算、气候变化评估和环境质量评价有着重要意义。

关 键 词:大气气溶胶  积聚模态比例  细模态Angstrom指数   
收稿时间:2013-01-28

Improving Accumulation-Mode Fraction Based on Spectral Aerosol Optical Depth in Beijing
ZHANG Ying,LI Zheng-qiang,WANG Yan,LI Kai-tao,LI Dong-hui,ZHANG Yu-huan,WEI Peng WANG Ling,Lü Yang. Improving Accumulation-Mode Fraction Based on Spectral Aerosol Optical Depth in Beijing[J]. Spectroscopy and Spectral Analysis, 2013, 33(10): 2795-2802. DOI: 10.3964/j.issn.1000-0593(2013)10-2795-08
Authors:ZHANG Ying  LI Zheng-qiang  WANG Yan  LI Kai-tao  LI Dong-hui  ZHANG Yu-huan  WEI Peng WANG Ling  Lü Yang
Affiliation:1. Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing 100101, China2. University of Chinese Academy of Sciences, Beijing 100049, China
Abstract:In the present study, the authors put forward a parameterization method of correcting fine-mode Angstrom index with aerosol optical depth and volume distribution of aerosol derived from AERONET in Beijing over 2011. The parameterization method is coupled with aerosol optical depth spectral deconvolution algorithm to improve the accuracy of accumulation-mode fraction. The errors of estimated AMF are derived from underestimate of fine-mode Angstrom index errors. We calculate and simulate the extreme values of fine-mode Angstrom index, getting constraint conditions, and then establish the extreme values correction method. Results from sensitivity test suggest that extreme values of fine-mode Angstrom index are constrained in the reasonable range. Fine-mode Angstrom index and AMF are sensitive to normalized volume distribution of aerosol, ranging from 0.662 to 2.849 and from 0.08 to 0.84 due to different distribution. Mean deviation of accumulation-mode fraction is reduced from 0.072 to 0.044, and the difference is 38.89%, especially in winter and summer. Improving computational accuracy of accumulation-mode fraction can enhance that of anthropogenic aerosol optical thickness, and it has important significance of anthropogenic aerosol direct radiation force estimation and environmental quality assessment.
Keywords:Atmospheric aerosol  Accumulation-mode fraction  Fine-mode Angstrom index
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