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Automated compact mobile Raman lidar for water vapor measurement: instrument description and validation by comparison with radiosonde, GNSS, and high-resolution objective analysis

机译:用于水蒸气测量的自动紧凑型移动拉曼LIDAR:仪器描述和验证与无线电探测器,GNSS和高分辨率目标分析相比

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摘要

We developed an automated compact mobile Raman lidar (MRL) system for measuring the vertical distribution of the water vapor mixing ratio (w) in the lower troposphere, which has an affordable cost and is easy to operate. The MRL was installed in a small trailer for easy deployment and can start measurement in a few hours, and it is capable of unattended operation for several months. We describe the MRL system and present validation results obtained by comparing the MRL-measured data with collocated radiosonde, Global Navigation Satellite System (GNSS), and high-resolution objective analysis data. The comparison results showed that MRL-derived w agreed within 10% (root-mean-square difference of 1.05 gkg(-1)) with values obtained by radiosonde at altitude ranges between 0.14 and 1.5 km in the daytime and between 0.14 and 5-6 km at night in the absence of low clouds; the vertical resolution of the MRL measurements was 75-150 m, their temporal resolution was less than 20 min, and the measurement uncertainty was less than 30 %. MRL-derived precipitable water vapor values were similar to or slightly lower than those obtained by GNSS at night, when the maximum height of MRL measurements exceeded 5 km. The MRL-derived w values were at most 1 gkg(-1) (25 %) larger than local analysis data. A total of 4 months of continuous operation of the MRL system demonstrated its utility for monitoring water vapor distributions in the lower troposphere.
机译:我们开发了一种自动紧凑型移动拉曼LIDAR(MRL)系统,用于测量较低对流层中水蒸气混合比(W)的垂直分布,这具有实惠的成本并且易于操作。 MRL安装在小型拖车中,以便于部署,可以在几个小时内开始测量,并且能够无人看管的操作数月。我们描述了MRL系统,并通过将MRL测量数据与配套无线电探空器,全局导航卫星系统(GNSS)和高分辨率目标分析数据进行比较来获得的MRL系统和目前的验证结果。比较结果表明,MRL-衍生的W在10%内(1.05 gkg(-1)的根平均平方差异),在白天的高度范围内通过无线电探测仪获得的值在0.14和1.5公里之间,在0.14和5之间。在没有低云的夜间6公里; MRL测量的垂直分辨率为75-150米,它们的时间分辨率小于20分钟,测量不确定度小于30%。当MRL测量的最大高度超过5km时,MRL衍生的可沉淀水蒸气值类似于或略低于夜间通过GNSS获得的水蒸气值。 MRL衍生的W值最多比局部分析数据大于1 GKG(-1)(25%)。总共4个月的MRL系统的连续操作证明了其用于监测较低对流层中的水蒸气分布的实用性。

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  • 来源
    《Atmospheric Measurement Techniques》 |2019年第1期|共14页
  • 作者单位

    Meteorol Res Inst Meteorol Satellite &

    Observat Syst Res Dept Tsukuba Ibaraki 3050052 Japan;

    Meteorol Res Inst Meteorol Satellite &

    Observat Syst Res Dept Tsukuba Ibaraki 3050052 Japan;

    Japan Meteorol Agcy Observat Dept Chiyoda Ku 1-3-4 Otemachi Tokyo 1008122 Japan;

    Meteorol Res Inst Meteorol Satellite &

    Observat Syst Res Dept Tsukuba Ibaraki 3050052 Japan;

    Meteorol Res Inst Meteorol Satellite &

    Observat Syst Res Dept Tsukuba Ibaraki 3050052 Japan;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 计量学;
  • 关键词

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