Manzo Matteo, Aiesi Gianpiero, Boselli Antonella, Consoli Salvatore, Damiano Riccardo, Di Donfrancesco Guido, Saraceno Benedetto, Scollo Simona
Dipartimento di Fisica "Ettore Pancini", Università di Napoli Federico II, Complesso Universitario di Monte S. Angelo, 80126 Napoli, Italy.
Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Piazza Roma 2, 95125 Catania, Italy.
Sensors (Basel). 2024 Mar 8;24(6):1762. doi: 10.3390/s24061762.
An innovative mobile lidar device, developed to monitor volcanic plumes during explosive eruptions at Mt. Etna (Italy) and to analyse the optical properties of volcanic particles, was upgraded in October 2023 with the aim of improving volcanic plume retrievals. The new configuration of the lidar allows it to obtain new data on both the optical and the microphysical properties of the atmospheric aerosol. In fact, after the upgrade, the lidar is able to measure three backscattering coefficients, two extinction coefficients and two depolarisation ratios in a configuration defined as "state-of-the-art lidar", where properties such as particle size distribution and the refractive index can be derived. During the lidar implementation, we were able to test the system's performance through specific calibration measurements. A comparison in an aerosol-free region (7.2-12 km) between lidar signals at 1064 nm, 532 nm and 355 nm and the corresponding pure molecular profiles showed a relative difference of <1% between them for all the wavelengths, highlighting the good dynamic of the signals. The overlap correction allowed us to reduce the underestimation of the backscattering coefficient from 50% to 10% below 450 m and 750 m at both 355 and 532 nm, respectively. The correct alignment between the laser beam and the receiver optical chain was tested using the signal received from the different quadrants of the telescope, and the relative differences between the four directions were comparable to zero, within the margin of error. Finally, the first measurement results are shown and compared with results obtained by other instruments, with the aim of proving the ability of the upgraded system to more precisely characterise aerosol optical and microphysical properties.
一种创新的移动激光雷达设备,旨在监测意大利埃特纳火山爆发期间的火山羽流并分析火山颗粒的光学特性,于2023年10月进行了升级,目的是改进火山羽流反演。激光雷达的新配置使其能够获取有关大气气溶胶光学和微物理特性的新数据。事实上,升级后,激光雷达能够在一种被定义为“最先进激光雷达”的配置中测量三个后向散射系数、两个消光系数和两个偏振比,从中可以推导出诸如粒径分布和折射率等特性。在激光雷达实施过程中,我们能够通过特定的校准测量来测试系统性能。在无气溶胶区域(7.2 - 12千米)对1064纳米、532纳米和355纳米处的激光雷达信号与相应的纯分子剖面进行比较,结果表明所有波长下它们之间的相对差异均小于1%,突出了信号的良好动态特性。重叠校正使我们能够将355纳米和532纳米处分别在450米和750米以下的后向散射系数低估从50%降低到10%。利用从望远镜不同象限接收到的信号测试了激光束与接收器光链之间的正确对准,四个方向之间的相对差异在误差范围内与零相当。最后,展示了首次测量结果并与其他仪器获得的结果进行比较,目的是证明升级后的系统更精确地表征气溶胶光学和微物理特性的能力。