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首页> 外文期刊>Atmospheric chemistry and physics >Ground-based water vapour soundings by microwave radiometry and Raman lidar on Jungfraujoch (Swiss Alps)
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Ground-based water vapour soundings by microwave radiometry and Raman lidar on Jungfraujoch (Swiss Alps)

机译:少女峰(瑞士阿尔卑斯山)上的微波辐射测量和拉曼激光雷达探测地面水汽探测

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Water vapour has been measured from the International Scientific StationJungfraujoch (ISSJ, 47° N, 7° E, 3580m above sealevel) during the winters of 1999/2000 and 2000/2001 by microwave radiometryand Raman lidar. The abundance of atmospheric water vapour between theplanetary boundary layer and the upper stratosphere varies over more thanthree orders of magnitude. The currently used measurement techniques are onlysuited to determine the abundance of water vapour in different atmosphericregimes. None can resolve the vertical distribution profile from groundlevel to the top of the stratosphere by itself. We present such a watervapour profile where simultaneous measurements from a Raman lidar and amicrowave radiometer were combined to cover both the troposphere and thestratosphere, respectively. We also present a study of the stratospheric andtropospheric water vapour variability for the two consecutive winters.
机译:在1999/2000年和2000/2001年冬季,通过微波辐射测定法和拉曼激光雷达,从少女峰国际科学站(ISSJ,北纬47°,东经7°,海拔3580m)测量了水汽。在行星边界层和高平流层之间的大气水蒸气的丰度变化超过三个数量级。当前使用的测量技术仅适用于确定不同大气条件下水蒸气的丰度。没有人能够单独解决从地平面到平流层顶部的垂直分布轮廓。我们提出了这样一种水蒸气剖面,其中同时进行了拉曼激光雷达和微波辐射仪的同时测量,以分别覆盖对流层和平流层。我们还提出了对两个连续冬季平流层和对流层水汽变异性的研究。

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