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Evaluation of the Lidar-Radar Cloud Ice Water Content Retrievals Using Collocated in Situ Measurements

机译:激光雷达-雷达云冰含量反演的评估

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摘要

Remote sensing and in situ measurements made during the Colorado Airborne Multiphase Cloud Study, 2010-2011 (CAMPS) with instruments aboard the University of Wyoming King Air aircraft are used to evaluate lidar-radar-retrieved cloud ice water content (IWC). The collocated remote sensing and in situ measurements provide a unique dataset for evaluation studies. Near-flight-level IWC retrieval is compared with an in situ probe: the Colorado closed-path tunable diode laser hygrometer (CLH). Statistical analysis showed that the mean radar-lidar IWC is within 26% of the mean in situ measurements for pure ice clouds and within 9% for liquid-topped mixed-phase clouds. Considering their different measurement techniques and different sample volumes, the comparison shows a statistically good agreement and is close to the measurement uncertainty of the CLH, which is around 20%. It is shown that ice cloud microphysics including ice crystal shape and orientation has a significant impact on IWC retrievals. These results indicate that the vertical profile of the retrieved lidar-radar IWC can be reliably combined with the flight-level measurements made by the in situ probes to provide a more complete picture of the cloud microphysics.
机译:在怀俄明国王航空大学的飞机上进行的2010-2011年科罗拉多州航空多相云研究(CAMPS)中进行的遥感和原位测量,用于评估激光雷达雷达释放的云冰水含量(IWC)。并置的遥感和原位测量为评估研究提供了唯一的数据集。将近飞行水平的IWC取回与现场探头进行比较:Colorado闭路可调谐二极管激光湿度计(CLH)。统计分析表明,纯冰云的平均雷达-雷达IWC值在原位平均测量值的26%以内,而液顶混合相云的平均值在9%以内。考虑到它们不同的测量技术和不同的样品量,该比较显示出统计上的良好一致性,并且接近CLH的测量不确定度,约为20%。结果表明,冰云的微观物理学包括冰晶的形状和取向对IWC的取回有重要影响。这些结果表明,可以将检索到的激光雷达-雷达IWC的垂直剖面与原位探测器进行的飞行高度测量可靠地结合起来,从而提供更完整的云微物理学图景。

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