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Recommendations for processing atmospheric attenuated backscatter profiles from Vaisala CL31 ceilometers

机译:维萨拉CL31云高仪对处理大气衰减反向散射剖面的建议

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摘要

Ceilometer lidars are used for cloud base height detection, to probe aerosol layers in the atmosphere (e.g. detection of elevated layers of Saharan dust or volcanic ash), and to examine boundary layer dynamics. Sensor optics and acquisition algorithms can strongly influence the observed attenuated backscatter profiles; therefore, physical interpretation of the profiles requires careful application of corrections. This study addresses the widely deployed Vaisala CL31 ceilometer. Attenuated backscatter profiles are studied to evaluate the impact of both the hardware generation and firmware version. In response to this work and discussion within the CL31/TOPROF user community (TOPROF, European COST Action aiming to harmonise ground-based remote sensing networks across Europe), Vaisala released new firmware (versions 1.72 and 2.03) for the CL31 sensors. These firmware versions are tested against previous versions, showing that several artificial features introduced by the data processing have been removed. Hence, it is recommended to use this recent firmware for analysing attenuated backscatter profiles. To allow for consistent processing of historic data, correction procedures have been developed that account for artefacts detected in data collected with older firmware. Furthermore, a procedure is proposed to determine and account for the instrument-related background signal from electronic and optical components. This is necessary for using attenuated backscatter observations from any CL31 ceilometer. Recommendations are made for the processing of attenuated backscatter observed with Vaisala CL31 sensors, including the estimation of noise which is not provided in the standard CL31 output. After taking these aspects into account, attenuated backscatter profiles from Vaisala CL31 ceilometers are considered capable of providing valuable information for a range of applications including atmospheric boundary layer studies, detection of elevated aerosol layers, and model verification.
机译:云高仪激光雷达用于云底高度检测,以探测大气中的气溶胶层(例如,检测撒哈拉尘埃或火山灰的升高层),并检查边界层动力学。传感器光学器件和采集算法会极大地影响观察到的衰减后向散射曲线。因此,对轮廓的物理解释需要仔细应用校正。这项研究针对的是广泛部署的维萨拉CL31云高仪。研究了衰减后向散射曲线,以评估硬件生成和固件版本的影响。为了响应CL31 / TOPROF用户社区(TOPROF,旨在协调整个欧洲地面遥感网络的欧洲COST行动)中的工作和讨论,维萨拉发布了CL31传感器的新固件(版本1.72和2.03)。这些固件版本已针对以前的版本进行了测试,表明已删除了数据处理引入的一些人工功能。因此,建议使用此最新固件来分析衰减的反向散射轮廓。为了对历史数据进行一致的处理,已开发出纠正程序,以解决在使用较旧固件收集的数据中检测到的伪影。此外,提出了一种程序来确定和说明来自电子和光学组件的与仪器相关的背景信号。这对于使用来自任何CL31云高仪的衰减后向散射观测是必要的。建议对使用Vaisala CL31传感器观察到的衰减后向散射进行处理,其中包括标准CL31输出中未提供的噪声估计。在考虑了这些方面之后,维萨拉CL31云高仪的衰减后向散射剖面被认为能够为一系列应用提供有价值的信息,包括大气边界层研究,升高的气溶胶层检测和模型验证。

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