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Evaluation of the Interpretation of Ceilometer Data with RASS and Radiosonde Data

机译:利用RASS和探空仪数据评估云高仪数据的解释

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Since 2006 different remote monitoring methods for determining mixing-layer height have been operated in parallel in Augsburg (Germany). One method is based on the operation of eye-safe commercial mini-lidar systems (ceilometers). The optical backscatter intensities recorded with ceilometers provide information about the range-dependent aerosol concentration; gradient minima within this profile mark the tops of mixed layers. Special software for these ceilometers provides routine retrievals of lower atmospheric layering. A second method, based on sodar observations, detects the height of a turbulent layer characterized by high acoustic backscatter intensities due to thermal fluctuations and a high variance of the vertical velocity component. This information is extended by measurements with a radio-acoustic sounding system (RASS) that directly provides the vertical temperature profile from the detection of acoustic signal propagation and thus temperature inversions that mark atmospheric layers. Ceilometer backscatter information is evaluated by comparison with parallel measurements. Data are presented from 2 years of combined ceilometer and RASS measurements at the same site and from comparison with a nearby (60 km) radiosonde for larger-scale humidity information. This evaluation is designed to ensure mixing-layer height monitoring from ceilometer data more reliable.CT 15th International Symposium for the Advancement of Boundary-Layer Remote Sensing (ISARS)CY JUN 28-30, 2010CL Univ Versailles St-Quentin-en-Yvelines, Inst Pierre Simon Laplace (IPSL), Paris, FRANCEHO Univ Versailles St-Quentin-en-Yvelines, Inst Pierre Simon Laplace (IPSL)SP Ecole Polytechnique; CASQY; Ctr Natl Etudes Spatiales (CNES); CNRS-INSU; EU Program COST; LATMOS; Lab Meteorol Dynamique (LMD); Leosphere; Meteo France; Reg Ile-de-France
机译:自2006年以来,用于确定混合层高度的不同远程监控方法已在奥格斯堡(德国)并行运行。一种方法是基于人眼安全的商用小型激光雷达系统(测高仪)的操作。用云高仪记录的光学反向散射强度提供了与范围相关的气溶胶浓度的信息。该轮廓内的梯度最小值标记了混合层的顶部。这些云高仪的专用软件可对较低的大气层进行常规检索。基于声雷达观测的第二种方法,检测湍流层的高度,该湍流层的特征是由于热波动和垂直速度分量的高变化而导致的高声学反向散射强度。通过使用无线电声探测系统(RASS)进行的测量可以扩展此信息,该系统可以从检测到的声信号传播以及标记大气层的温度反转直接提供垂直温度分布。云高仪反向散射信息是通过与并行测量进行比较来评估的。数据来自在同一地点进行的2年云高仪和RASS组合测量,以及与附近(60公里)探空仪进行比较以获取更大规模的湿度信息的数据。此评估旨在确保从云高仪数据进行的混合层高度监控更加可靠。CT第15届国际边界层遥感技术研讨会(ISARS),CY JUN,28-30,2010年,CL凡尔赛大学,圣昆汀恩-伊夫林省, Pierre Simon Laplace研究所(IPSL),巴黎,法国凡尔赛大学圣奎因恩伊夫林省,Pierre Simon Laplace研究所(IPSL)SP巴黎理工学院; CASQY; Ctr Natl Etudes Spatiales(CNES); CNRS-INSU;欧盟计划成本;拉莫斯Lab Meteorol Dynamique(LMD);狮子座法国Meteo;法兰西岛大区

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