| 霾期间上海低层气溶胶微物理属性与地面相对湿度分析 |
| |
| 引用本文： | 黄家敏,陈星宇,安静宇,杨洪海,陈勇航,王秀珍,张 华,冯帆,李 梦,刘岩.霾期间上海低层气溶胶微物理属性与地面相对湿度分析[J].新疆气象,2015,9(1):39-44. |
| |
| 作者姓名： | 黄家敏 陈星宇 安静宇 杨洪海 陈勇航 王秀珍 张 华 冯帆 李 梦 刘岩 |
| |
| 作者单位： | 东华大学环境科学与工程学院,东华大学环境科学与工程学院,东华大学环境科学与工程学院,东华大学环境科学与工程学院,东华大学环境科学与工程学院,杭州师范大学遥感与地球科学研究院,中国气象局国家气候中心,东华大学环境科学与工程学院,东华大学环境科学与工程学院,东华大学环境科学与工程学院 |
| |
| 基金项目： | 国家重点基础研究发展计划(No. 2011CB403405)；杭州市科技发展计划项目(20120433B18)；国家自然科学基金(No.40975012) |
| |
| 摘 要： | 用2007年1月至2010年11月美国国家航空航天局(NASA)的CALIPSO星载激光雷达资料,通过532 nm总后向散射系数、体积退偏比和色比,分析了上海地区霾期间低层0~2 km高度气溶胶微物理属性与地面相对湿度的关系。结果表明,当地面相对湿度为65%~80%时,后向散射系数在0~0.001 km-1·sr-1范围内出现的频率最大;当地面相对湿度为50%~65%时,后向散射系数大于0.001 km-1·sr-1的频率最大;低层大气中聚集的主要是规则气溶胶粒子,当地面相对湿度为65%~80%时,气溶胶粒子最为规则,其次为80%~95%的地面相对湿度。当地面相对湿度为50%~65%时,不规则气溶胶粒子所占比重较大;霾期间,低层大气中细粒子气溶胶均占主导地位,但随着地面相对湿度的增大,气溶胶粒子粒径逐渐增大。在地面相对湿度为80%~95%时,大颗粒气溶胶相对较多。
|
| 关 键 词： | 霾 相对湿度 气溶胶 CALIPSO 微物理属性 |
| 收稿时间： | 2014/5/19 0:00:00 |
| 修稿时间： | 2014/7/10 0:00:00 |
Analysis of Low-level Aerosol Microphysical Properties and Surface Relative Humidity during the Haze in Shanghai |
| |
| HUANG Jia-min,CHEN Yong-hang,AN Jing-yu,YANG Hong-hai,CHEN Yong-hang,WANG Xiuzhen,ZHANG Hu,ZHANG Hu,LI Meng and LIU Yan.Analysis of Low-level Aerosol Microphysical Properties and Surface Relative Humidity during the Haze in Shanghai[J].Bimonthly of Xinjiang Meteorology,2015,9(1):39-44. |
| |
| Authors: | HUANG Jia-min CHEN Yong-hang AN Jing-yu YANG Hong-hai CHEN Yong-hang WANG Xiuzhen ZHANG Hu ZHANG Hu LI Meng and LIU Yan |
| |
| Institution: | College of Environmental Science and Engineering, Donghua University,College of Environmental Science and Engineering, Donghua University,College of Environmental Science and Engineering, Donghua University,College of Environmental Science and Engineering, Donghua University,College of Environmental Science and Engineering, Donghua University,Remote Sensing and Earth Sciences Research Institute, Hangzhou Normal University,National Climate Center of China Meteorological Administration,College of Environmental Science and Engineering, Donghua University, No. 2999, North Renmin Road, Songjiang District, Shanghai,College of Environmental Science and Engineering, Donghua University,College of Environmental Science and Engineering, Donghua University |
| |
| Abstract: | Based on the onboard lidar data from CALIPSO satellite of National Aeronautics and Space Administration (NASA) from January 2007 to November 2010, the relationship between 0-2km altitude aerosol microphysical properties and surface relative humidity of lower troposphere during the haze in Shanghai were revealed by analyzing the parameters of 532nm total attenuated backscatter coefficient, volume depolarization ratio and total attenuated color ratio. The results showed that when the 532nm backscattering coefficient was in the range of 0 to 0.001 km-1?sr-1, the frequency of 532nm backscattering coefficient was the largest with the surface relative humidity was 65%-80%, while when the 532nm backscattering coefficient was greater than 0.001 km-1?sr-1, its frequency reached the maximum with the surface relative humidity was 50%-65%. The main constituents of lower troposphere were regular aerosols and the most regular aerosols appeared on the relative humidity was within 65%-80% while the most irregular aerosols appeared on the relative humidity was within 50%-65%. In addition, fine particle aerosols were the dominant aerosols of lower troposphere in the haze. With the increase of surface relative humidity, the aerosol particle size increased, and the proportion of large aerosols were highest when the surface relative humidity was within 80%-95%. |
| |
| Keywords: | haze relative humidity aerosol CALIPSO microphysical properties |
| 本文献已被 CNKI 等数据库收录！ |
| 点击此处可从《新疆气象》浏览原始摘要信息 |
| 点击此处可从《新疆气象》下载免费的PDF全文 |
|
