杨辉, 李新建, 陈培彬, 宗军君, 刘剑, 刘文清. 青藏高原对流层气溶胶的激光雷达监测与研究[J]. 应用光学, 2013, 34(3): 507-511.
引用本文: 杨辉, 李新建, 陈培彬, 宗军君, 刘剑, 刘文清. 青藏高原对流层气溶胶的激光雷达监测与研究[J]. 应用光学, 2013, 34(3): 507-511.
YANG Hui, LI Xin-jian, CHEN Pei-bin, ZONG Jun-jun, LIU Jian, LIU Wen-qing. Monitoring and study of tropospheric aerosol by lidar over Tibet plateau[J]. Journal of Applied Optics, 2013, 34(3): 507-511.
Citation: YANG Hui, LI Xin-jian, CHEN Pei-bin, ZONG Jun-jun, LIU Jian, LIU Wen-qing. Monitoring and study of tropospheric aerosol by lidar over Tibet plateau[J]. Journal of Applied Optics, 2013, 34(3): 507-511.

青藏高原对流层气溶胶的激光雷达监测与研究

Monitoring and study of tropospheric aerosol by lidar over Tibet plateau

  • 摘要: 运用激光雷达方程和Fernald方法,对西藏那曲地区和北京地区对流层气溶胶的微脉冲激光雷达(MPL)探测数据进行时空反演和比较,结果表明:气溶胶散射比廓线有着较为相似的结构分布,分层锯齿结构非常明显,主要包括贴地层、气溶胶混合层和气溶胶对流层。那曲测站上空气溶胶散射比在无云条件下最大值基本上保持在2.0左右;在测站上空均存在密度较大且较厚的积云;夏季的混合层或残留层(浅蓝色部分)高度抬高;夏季对流层低层积云的云量和积云出现的概率较冬季要少。

     

    Abstract: Qinghai-Tibet plateau is famous for the name of the third pole of the earth. The aerosol vertical scattering ratio profiles and extinction coefficient time-space distribution at Naqu prefecture and Beijing prefecture were shown and compared. The data shows that: the similar multi-layered zigzag vertical structure of aerosol extinction coefficient distribution exists in the day and night time; the layers include close ground layer, mixed layer and troposphere. The maximum value of aerosol scattering ratio remains at 2.0 under cloud-free conditions. Because of the vapor cycle, cumulus is existed over the prefecture most of the time, and presence probability of cumulus in summer is less than in winter.

     

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