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Results of the study of variability of the background aerosol content in the stratosphere over Tomsk based on the data of lidar measurements in 2011 – 2015

机译:基于2011年至2015年激光雷达测量数据的平流层上托木斯克地区背景气溶胶含量变化的研究结果

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The experimental results on the variability of the vertical-temporal structure of the stratospheric aerosol over Tomsk,obtained at the lidar complex of the Small Lidar Station of IAO of the SB RAS in the period 2011-2015 are presented.The characteristic peculiarity of this period, except of the second half of 2011, (appearance of the eruptive layers of theGrimsvotn volcano eruption over Tomsk) was practical absence of volcanic activity leading to the formation ofstratospheric aerosol and its transfer to Tomsk, and therefore it became possible to study the behavior of the verticalstructure of the background aerosol in the stratosphere during five years. According to the analysis of the lidar dataobtained, a stable trend of aerosol filling of the lower stratosphere during the cold season with its maximum content inDecember-January and a practical absence of aerosol in the entire stratosphere layer during the warm season wasrevealed.
机译:提出了关于托木斯克平流层气溶胶垂直时空结构变化的实验结果,这是在2011-2015年期间在SB RAS IAO小激光雷达站的激光雷达综合体上获得的。 n除2011年下半年外,这一时期的特征是特殊的(托木斯克\ r \ n格里姆斯沃特火山喷发的出现),实际上没有火山活动,导致了\ r \ n平流层气溶胶及其形成转移到托木斯克,因此有可能研究五年内平流层背景气溶胶垂直结构的行为。根据获得的激光雷达数据分析,在寒冷季节,平流层下部的气溶胶填充趋势稳定,在12月至1月其含量最高,而平流层整个层实际上都没有气溶胶。温暖的季节被揭露了。

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