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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Evaluating lidar-radar microphysics retrieval using in situ measurements
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Evaluating lidar-radar microphysics retrieval using in situ measurements

机译:使用原位测量评估激光雷达-雷达微观物理学检索

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摘要

This study reports on a comparison between in situ and combined lidar and radar measurements of extinction and ice water content in ice clouds. The main goal of this exercise is to verify that the lidar-radar method can be confidently used for future satellite radar and lidar measurements. The data used in this study were obtained during the Cirrus Regional Study of Tropical Anvils and Cirrus Layers–Florida Area Cirrus Experiment (CRYSTAL-FACE) campaign that was conducted to study the properties of low-latitude, continentally influenced ice cloud layers. Two different methods are used to retrieve the extinction from the lidar signal. The comparison between lidar-derived and in situ–derived extinction values shows that they are strongly correlated for the two different lidar-based methods. Linear fits between the ice water contents derived from the two extinctions and radar reflectivity and the in situ values result in slope parameters of 0.93 ± 0.28 and 1.09 ± 0.35. The precise values depend on the assumed ice particle properties and particle size distribution used in the lidar-radar retrievals.
机译:这项研究报告了在原位与组合激光雷达和雷达测量消光和冰云中冰水含量之间的比较。本练习的主要目的是验证激光雷达-雷达方法可以可靠地用于未来的卫星雷达和激光雷达测量。本研究中使用的数据是在热带铁砧和卷云的卷云区域研究–佛罗里达地区卷云实验(CRYSTAL-FACE)活动中获得的,该活动旨在研究低纬度,受大陆影响的冰云层的特性。两种不同的方法用于从激光雷达信号中恢复消光。激光雷达消光值与原位消光值之间的比较表明,对于两种基于激光雷达的方法,它们具有极强的相关性。两次消光产生的冰水含量与雷达反射率之间的线性拟合以及原位值得出的斜率参数分别为0.93±0.28和1.09±0.35。精确值取决于在激光雷达-雷达检索中使用的假定的冰粒特性和粒径分布。

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