首页 | 官方网站   微博 | 高级检索  
     

2009年上海浦东新区能见度资料的深度分析——兼论高时间分辨率地面观测资料的应用
引用本文:毕 凯,王广河,毛节泰.2009年上海浦东新区能见度资料的深度分析——兼论高时间分辨率地面观测资料的应用[J].气象,2012,38(2):220-227.
作者姓名:毕 凯  王广河  毛节泰
作者单位:1. 中国气象科学研究院人工影响天气中心,北京100081/北京市人工影响天气办公室,北京100089
2. 中国气象科学研究院人工影响天气中心,北京,100081
3. 北京大学物理学院大气科学系,北京,100871
基金项目:国家科技支撑计划项目(2006BAC12B04)、中国气象局行业专项(GYHY201106031,GYHY201006011)、国家重点基础研究发展计划项目(2011CB403401)共同资助
摘    要:利用2009年上海浦东新区气象站高时间分辨率的能见度资料及其同步地面气象要素资料,在气块静力稳定的假设下研究了由于辐射冷却引起的霾或雾在演变的各阶段气溶胶吸湿性增长及其消光系数随相对湿度的变化,结果表明:气溶胶吸湿性增长率f(RH)随相对湿度的增长具有先慢后快平滑连续的特点;气溶胶吸湿性增长率在不同季节有所差异,在夏季和秋季较高,在冬季和春季时较低;平均而言,当相对湿度从40%增大到95%时,气溶胶吸湿性增长率可达6.6;对比国内外实验和观测结果,发现f(RH)随相对湿度的变化曲线与硫酸铵亲水增长相似;在这种雾消散时,随着气温的升高,测量给出的相对湿度值不会立即下降,而是在接近饱和的情况下维持一段时间,然后再迅速下降,其滞后大约为1~2小时。这很可能是测湿元件不能及时反映外界湿度变化所致。

关 键 词:能见度  水汽密度  气溶胶  吸湿性增长率
收稿时间:2010/11/7 0:00:00
修稿时间:9/5/2011 12:00:00 AM

In-Depth Analysis on Atmospheric Visibility in Shanghai Pudong 2009——Concurrently on Applying Surface Meteorological Data with High Temporal Resolution
Bi Kai,Wang Guanghe and Mao Jietai.In-Depth Analysis on Atmospheric Visibility in Shanghai Pudong 2009——Concurrently on Applying Surface Meteorological Data with High Temporal Resolution[J].Meteorological Monthly,2012,38(2):220-227.
Authors:Bi Kai  Wang Guanghe and Mao Jietai
Affiliation:Weather Modification Center, Chinese Academy of Meteorological Sciences, Beijing 100081;Beijing Weather Modification Office, Beijing 100089;Weather Modification Center, Chinese Academy of Meteorological Sciences, Beijing 100081;Department of Atmospheric Science, Physics College, Peking University, Beijing 100871
Abstract:The absorption of water by ambient aerosols and the influence of ambient relative humidity on the extinction coefficient are investigated under the assumptions that the atmosphere is in static stability during low visibility process caused by radiative cooling using the continuous observations data(visibility, relative humidity,temperature,wind etc.) from Shanghai Pudong automatic weather stations in 2009. The subtle features of meteorological elements are also studied with such high temporal resolution(1 min) data.The results show that the hygroscopic growth factor f(RH) of the extinction coefficient increased continuously with RH and featured a first-slow-then-quick uptrend.The curves obtained from different seasons show that f(RH) was relatively higher in summer and autumn than that in winter and spring. Overall,the average f(RH) in 7 cases could reach to 6.6 when RH increased from less than 40%to 95%. We also present comparisons with other researches in the world,and the result shows that the behavior of the average of hygroscopic growth factor of the extinction coefficient in the cases is similar to the calculated growth factor of the scattering coefficient for ammonium sulfate.Further study also shows that the decrease of relative humidity is lagging about 1—2 hours behind the increase of temperature and visibility, which is conjectured that the humidity sensor fails to change quickly enough to measure the variation of relative humidity of the local air mass.
Keywords:visibility    vapor density    aerosol    hygroscopic growth factor
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《气象》浏览原始摘要信息
点击此处可从《气象》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司    京ICP备09084417号-23

京公网安备 11010802026262号