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Intercomparison of wind observations from the European Space Agency's Aeolus satellite mission and the ALADIN Airborne Demonstrator

机译:来自欧洲航天局的风析卫星卫星使命和阿拉丁机载示范仪的互相同步

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Shortly after the successful launch of the European Space Agency's wind mission Aeolus, co-located airborne wind lidar observations were performed in central Europe; these observations employed a prototype of the satellite instrument – the ALADIN (Atmospheric LAser Doppler INstrument) Airborne Demonstrator (A2D). Like the direct-detection Doppler wind lidar on-board Aeolus, the A2D is composed of a frequency-stabilized ultra-violet (UV) laser, a Cassegrain telescope and a dual-channel receiver to measure line-of-sight (LOS) wind speeds by analysing both Mie and Rayleigh backscatter signals. In the framework of the first airborne validation campaign after the launch and still during the commissioning phase of the mission, four coordinated flights along the satellite swath were conducted in late autumn of 2018, yielding wind data in the troposphere with high coverage of the Rayleigh channel. Owing to the different measurement grids and LOS viewing directions of the satellite and the airborne instrument, intercomparison with the Aeolus wind product requires adequate averaging as well as conversion of the measured A2D LOS wind speeds to the satellite LOS (LOS*). The statistical comparison of the two instruments shows a positive bias (of 2.6 m s?1) of the Aeolus Rayleigh winds (measured along its LOS*) with respect to the A2D Rayleigh winds as well as a standard deviation of 3.6 m s?1. Considering the accuracy and precision of the A2D wind data, which were determined from comparison with a highly accurate coherent wind lidar as well as with the European Centre for Medium-Range Weather Forecasts (ECMWF) model winds, the systematic and random errors of the Aeolus LOS* Rayleigh winds are 1.7 and 2.5 m s?1 respectively. The paper also discusses the influence of different threshold parameters implemented in the comparison algorithm as well as an optimization of the A2D vertical sampling to be used in forthcoming validation campaigns.
机译:在欧洲航天局的欧洲航天局的风调务通风公司成功推出后不久,共同位于中欧的空中风潮观测;这些观察结果采用卫星仪器的原型 - 阿拉丁(大气激光多普勒仪器)空气传播演示(A2D)。与直接检测多普勒风延线滑翔机一样,A2D由频率稳定的超紫(UV)激光器组成,Cassegrain望远镜和双通道接收器来测量视线(LOS)风通过分析MIE和RAYLEIGH反向散射信号来速度。在发布后第一次机载验证活动的框架中,仍在使命的调试阶段,沿着卫星条款的四次协调航班在2018年深度秋季进行,在对流层中产生风数据,瑞利渠道高覆盖范围。由于卫星和空中仪器的不同测量网格和洛氏观察方向,与Aeolus风产品的相互作用需要足够的平均以及测量的A2D LOS风速转换为卫星LOS(LOS *)。这两个仪器的统计比较显示了A2D瑞利风的A2D Rayleigh风(沿其LOS *测量的2.6米S'1)的正偏差(沿其LOS *测量)以及3.6米S的标准偏差。考虑到A2D风数据的准确性和精度,从与高度精确的相干风潮以及欧洲中距离(ECMWF)模型风的比较确定,欧洲的中距离(ECMWF)模型风,系统和随机误差LOS *瑞利风分别为1.7和2.5 m s?1。本文还讨论了在比较算法中实现的不同阈值参数的影响以及在即将到来的验证广告系列中使用的A2D垂直采样的优化。

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