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Lidar Measurements of Tropospheric Ozone over Reunion Island: Influence of the Synoptic Situations

机译:雷尼昂岛对流层臭氧的激光乐节测量:概要情况的影响

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A tropospheric ozone lidar located at Reunion Island has provided an opportunity to investigate the daily vertical ozone distribution in the latter part of biomass burning season, during November-December 1999. The comparison with austral winter 1998 daily ozone profiles show that each daily ozone profile is very stratified with ozone enhancements (<100 ppbv) spaced at different heights within the whole free troposphere. The dynamical context of the profiles is different in comparison with the austral winter period where the effect of the subtropical jet stream is predominant. The analyses of the meteorological data show that the daily variability of ozone profiles is influenced by the movement of the synoptical situations. During the interseasonal period, multiple ozone sources including stratosphere-troposphere exchanges, convection and biomass burning contribute to tropospheric ozone at Reunion Island through sporadic events characterized by a large spatial and temporal variability.
机译:位于Reunion Island的TroposhiC臭氧Lidar提供了机会,可以在1999年11月 - 12月期间调查后半部分燃烧季节的日常垂直臭氧分布。与澳大利亚冬季的比较1998年每日臭氧配置文件显示每次臭氧概况在整个自由对流层内的不同高度下间隔开的臭氧增强(<100 ppbv)非常分层。与亚热带射流效应是主要的澳大利亚冬季,曲线的动力背景与亚冬季冬季的冬季期不同。气象数据的分析表明,臭氧谱的日常变异性受到概要情况的运动的影响。在季期期期间,多个臭氧来源,包括平流层 - 对流层交换,对流和生物量燃烧,通过散发性岛屿来促成零星岛的对流层臭氧,其特征在于具有大的空间和时间变异性。

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