...
首页> 外文期刊>Atmospheric chemistry and physics >Cluster analysis of the impact of air back-trajectories on aerosol optical properties at Hornsund, Spitsbergen
【24h】

Cluster analysis of the impact of air back-trajectories on aerosol optical properties at Hornsund, Spitsbergen

机译:斯匹次卑尔根霍恩松德空气后向轨迹对气溶胶光学特性影响的聚类分析

获取原文
           

摘要

In this paper, spectra of aerosol optical thickness from the AERONET(AErosol RObotic NETwork) station at Hornsund in the southern partof Spitsbergen were employed to study the impact of air mass historyon aerosol optical thickness for wavelength λ=500 nm –AOT(500) – and the ?ngstr?m exponent. Backward trajectoriescomputed, using the NOAA HYSPLIT model, were used to trace airhistory. It was found that in spring, the changes in AOT values overthe Hornsund station were strongly influenced by air masstrajectories 8 days or longer in duration, arriving both in the freetroposphere and at an altitude of 1 km above sea level.Nevertheless, free tropospheric advection was dominant. AOTvariability in summer was best explained by the local direction andspeed of advection (1-day trajectories) and was dominated by theeffectiveness of cleansing processes. During the ASTAR 2007campaign, the aerosols near Hornsund displayed low AOT valuesranging from 0.06 to 0.09, which is lower than the mean AOT(500) forspring seasons from 2005 to 2007 (0.110±0.007; mean ±standard deviation of mean). 9 April 2007 with AOT(500)=0.147 wasexceptional. The back-trajectories belonged to clusters with low andaverage cluster mean AOT. Apart from the maximum AOT of9 April 2007, the observed AOT values were close to or lower thanthe means for the clusters to which they belonged.
机译:本文利用斯匹次卑尔根南部霍恩松德的AERONET(AErosol机器人网络)站的气溶胶光学厚度光谱研究了空气质量历史对波长λ= 500 nm的气溶胶光学厚度的影响–AOT(500)–和ngstr?m指数。使用NOAA HYSPLIT模型计算的后向轨迹用于追踪航空历史。发现在春季,霍恩松德站上空的AOT值的变化受到持续8天或更长时间的空气质量轨迹的强烈影响,这些运动既到达了对流层又到达了海拔1 km的高度。优势。夏季AOT的变化最好用对流的局部方向和速度(1天的轨迹)来解释,并且以清洁过程的有效性为主导。在2007年ASTAR活动期间,Hornsund附近的气溶胶显示出较低的AOT值,范围从0.06到0.09,低于2005年至2007年春季的平均AOT(500)(0.110±0.007;平均值的平均值±标准差)。 2007年4月9日,AOT(500)= 0.147是例外。反向轨迹属于具有低平均均值AOT的群集。除了2007年4月9日的最大AOT值外,观测到的AOT值接近或低于它们所属的群集的均值。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号