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10Be/7Be implies the contribution of stratosphere-troposphere transport to the winter-spring surface O3 variation observed on the Tibetan Plateau
Authors:Zheng  XiangDong  Shen  ChengDe  Wan  GuoJiang  Liu  KeXin  Tang  Jie  Xu  XiaoBin
Institution:ZHENG XiangDong* 1,SHEN ChengDe 2,WAN GuoJiang 3,LIU KeXin 4,TANG Jie 1 & XU XiaoBin 1 1 Chinese Academy of Meteorological Sciences,Beijing 100081,China,2 Key Laboratory of Isotope Geochronology and Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,3 State Key Laboratory of Environment Geochemistry,Institute of Geochemistry,Guiyang 550002,4 State Key laboratory of Nuclear Physics and Technology & Institute of Heavy Ion Physi...
Abstract:10Be/7Be is a stratospheric sensitive tracer. In this paper, measurements of 10Be/7Be and surface O3 from October 2005 to May 2006 at Mt. Waliguan (hereafter WLG, 100.898°E, 39.287°N, 3810 m, a.s.l.), China global atmospheric watch (GAW) observatory, are introduced and used to investigate the stratosphere-troposphere transport (STT) and its impact on surface O3 on the Tibetan Plateau. The results show that the magnitude of STT is weak in winter, followed by strengthening from the end of winter to the middle of spring (from mid February to mid April) with large increases in 10Be,7Be,10Be/7Be and surface O3. At the end of spring (from the end of April to mid May in this paper), the STT weakened, and the continuous increase of surface O3 at WLG is produced by tropospheric photochemistry reactions.
Keywords:10Be/7Be  stratosphere-troposphere transport  surface O3  Mt  Waliguan
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