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Radiation fog formation alerts using attenuated backscatter power from automatic lidars and ceilometers

机译:使用自动激光雷达和云高仪的衰减后向散射功率来生成辐射雾警报

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摘要

Radiation fog occurs over many locations around the world in stableatmospheric conditions. Air traffic at busy airports can be significantlydisrupted because low visibility at the ground makes it unsafe to take off,land and taxi on the ground. Current numerical weather prediction forecastsare able to predict general conditions favorable for fog formation, but notthe exact time or location of fog occurrence. A selected set of observationsavailable in near-real time at strategic locations could also be useful totrack the evolution of key processes and key parameters that drive fogformation. Such observations could complement the information predicted bynumerical weather prediction (NWP) models that is made available to airport forecasters in support of theirfog forecast. This paper presents an experimental setup based on collocatedautomatic lidar and ceilometer measurements, relative humidity measurementsand horizontal visibility measurements to study hygroscopic growth of fogcondensation nuclei. This process can take several minutes to hours, and canbe tracked using lidar- or ceilometer-attenuated backscatter profiles. Basedon hygroscopic growth laws we derive a set of parameters that can be used toprovide alerts minutes to hours prior to formation of radiation fog. Wepresent an algorithm that uses the temporal evolution of attenuatedbackscatter measurements to derive pre-fog formation alerts. The performanceof the algorithm is tested on 45 independent pre-fog situations at twolocations (near Paris, France, and Brussels, Belgium). We find that an alertfor pre-fog conditions predominantly occurs 10–50 min prior to fog formationat an altitude ranging 0 to 100 m above ground. In a few cases, alerts canoccur up to 100 min prior to fog formation. Alert durations are found to besensitive to the relative humidity conditions found a few hours prior to thefog.
机译:在稳定的大气条件下,世界各地的许多地方都会发生辐射雾。繁忙机场的空中交通可能会严重中断,因为地面低能见度使其在地面上起飞,降落和滑行都不安全。当前的数值天气预报能够预测有利于雾形成的一般条件,但不能预测雾发生的确切时间或位置。在战略位置近实时提供的一组选定观测值也可能有助于跟踪驱动雾形成的关键过程和关键参数的演变。这些观测结果可以补充由机场天气预报员提供的支持天气预报的数字天气预报(NWP)模型所预测的信息。本文提出了一种基于并置自动激光雷达和云高仪测量,相对湿度测量和水平能见度测量的实验装置,以研究雾凝核的吸湿性增长。此过程可能需要几分钟到几小时,并且可以使用激光雷达或云高仪衰减的反向散射剖面进行跟踪。根据吸湿性增长定律,我们得出了一组参数,可用于在辐射雾形成之前的几分钟到几小时内提供警报。我们提出一种算法,该算法使用衰减后向散射测量值的时间演变来导出雾前形成警报。该算法的性能在两个位置(法国巴黎附近和比利时布鲁塞尔附近)的45个独立的预雾情况下进行了测试。我们发现,在距地面0至100μm的海拔高度上,在雾形成之前10–50 min会发生预雾情况的警报。在少数情况下,警报可能会在雾形成之前长达100分钟出现。发现警报持续时间对在雾前几个小时发现的相对湿度条件敏感。

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