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Determination of boundary-layer parameters using wind profiler/RASS and sodar/RASS in the frame of the LITFASS project

机译:在LITFASS项目框架中使用风廓线仪/ RASS和声雷达/ RASS确定边界层参数

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Progress in technology as well as signal processing has promoted Wind Profiler Radar (WPR) or sodar with RASS additions to become standard tools in profiling of the atmospheric boundary layer. Apart from these instruments' basic abilities in profiling mean winds and temperature, this paper will give an emphasis on the profiling of ABL height as well as the turbulent fluxes of sensible heat and momentum both, with respect to methods as well as with respect to realization. The special focus will thereby be laid on the demands for vertical profiling, which were defined within the LITFASS-project of the German Meteorological Service. In the frame of this project, some special measuring campaigns have been performed where remote-sensing systems were used to assess their abilities in profiling ABL parameters. On the base of some case studies from these campaigns comparisons are shown, where results from sodar/RASS and WPR/RASS measurements are compared to measurements from airborne sensor systems and results from numerical models. Regarding turbulent heat fluxes, we found excellent agreement for remotely-sensed flux profiles from WPR/RASS with both, numerical models and airborne in-situ measurements. However, as the inherent errors of the remotely-sensed fluxes are in the order of +- 20 ... 30W/m~2 typically, current signal processing does not allow to interpret small-scale vertical structures in the profiles with respect to surface inhomogeneities yet.
机译:技术和信号处理的进步促进了Wind Profiler雷达(WPR)或声雷达与RASS的加入,已成为大气边界层轮廓分析的标准工具。除了这些仪器在分析平均风和温度方面的基本能力外,本文还将重点介绍ABL高度的分析以及显热和动量的湍流,包括方法和实现。 。因此,将特别关注垂直剖面的需求,这是德国气象局LITFASS项目中定义的。在该项目的框架中,已经进行了一些特殊的测量活动,其中使用遥感系统评估其在分析ABL参数方面的能力。在这些战役的一些案例研究的基础上,进行了比较,其中将声雷达/ RASS和WPR / RASS测量的结果与机载传感器系统的测量结果和数值模型的结果进行了比较。关于湍流热通量,我们发现WPR / RASS的遥感通量剖面与数值模型和机载现场测量都非常吻合。但是,由于遥感通量的固有误差通常在+/- 20 ... 30W / m〜2的数量级,因此电流信号处理无法解释轮廓中相对于表面的小规模垂直结构。还不均匀。

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