激光多普勒风速仪同时后向散射测量结果的改进

F. Köpp
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引用次数: 0

摘要

红外多普勒激光雷达系统已被证明对大气风和湍流的远程测量非常有效。在过去的五年中,DFVLR的连续波CO2激光多普勒风速仪(LDA)已经成功地用于不同的常规应用,例如,测量高达750米高度的垂直风廓线或接近海面的风廓线。另一类应用包括对湍流结构的研究,特别是对飞机尾流涡的探测和跟踪。尽管在这些和额外的实地试验中获得了所有准确的结果,但在不利的情况下,一些困难变得明显,可能影响LDA的测量。其中一种情况是在感应体内部或附近存在强烈散射层,如雾或低云。本文描述了使用后向散射激光雷达和云高仪同时测量气溶胶剖面和云高所产生的可能性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Improvement of laser Doppler anemometer results by simultaneous backscatter measurements
Infrared Doppler lidar systems have proven very efficient for remote measurements of atmospheric wind and turbulence. During the last five years the cw CO2 laser Doppler anemometer (LDA) from DFVLR has been successfully used for different routine applications, for example, the measurement of vertical wind profiles up to 750 m altitude or wind profiles close to the sea surface. Another type of applications covers the investigation of turbulence structures, especially the detection and tracking of aircraft wake vortices. Despite all the accurate results gained during these and additional field experiments, some difficulties became evident which can influence the LDA measurements in unfavourable cases. One of those cases is the presence of strongly scattering layers like fog or low clouds within or nearby the sensing volume. This paper describes the possibilities which arise by simultaneous measurements of aerosol profiles and cloud heights using a backscatter lidar and a ceilometer.
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