首页> 外文期刊>Journal of atmospheric and oceanic technology >The Airborne Demonstrator for the Direct-Detection Doppler Wind Lidar ALADIN on ADM-Aeolus. Part II: Simulations and Rayleigh Receiver Radiometric Performance
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The Airborne Demonstrator for the Direct-Detection Doppler Wind Lidar ALADIN on ADM-Aeolus. Part II: Simulations and Rayleigh Receiver Radiometric Performance

机译:ADM-Aeolus上的直接检测多普勒测风激光雷达ALADIN的机载演示器。第二部分:仿真和瑞利接收器的辐射性能

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In the frame of the Atmospheric Dynamics Mission Aeolus (ADM-Aeolus) satellite mission by the European Space Agency (ESA), a prototype of a direct-detection Doppler wind lidar was developed to measure wind from ground and aircraft at 355 nm. Wind is measured from aerosol backscatter signal with a Fizeau interferometer and from molecular backscatter signal with a Fabry-Perot interferometer. The aim of this study is to validate the satellite instrument before launch, improve the retrieval algorithms, and consolidate the expected performance. The detected backscatter signal intensities determine the instrument wind measurement performance among other factors, such as accuracy of the calibration and stability of the optical alignment. Results of measurements and simulations for a ground-based instrument are compared, analyzed, and discussed. The simulated atmospheric aerosol models were validated by use of an additional backscatter lidar. The measured Rayleigh backscatter signals of the wind lidar prototype up to an altitude of 17 km are compared to simulations and show a good agreement by a factor better than 2, including the analyses of different error sources. First analyses of the signal at the Mie receiver from high cirrus clouds are presented. In addition, the simulations of the Rayleigh signal intensities of the Atmospheric Laser Doppler Instrument (ALADIN) Airborne Demonstrator (A2D) instrument on ground and aircraft were compared to simulations of the satellite system. The satellite signal intensities above 11.5 km are larger than those from the A2D ground-based instrument and always smaller than those from the aircraft for all altitudes.
机译:在欧洲航天局(ESA)进行的大气动力学风神卫星(ADM-Aeolus)卫星任务的框架中,开发了一种直接探测多普勒风激光雷达的原型,以测量355海里来自地面和飞机的风。使用Fizeau干涉仪根据气溶胶反向散射信号测量风,使用Fabry-Perot干涉仪根据分子反向散射信号测量风。这项研究的目的是在发射前验证卫星仪器,改进检索算法并巩固预期性能。检测到的反向散射信号强度决定了仪器风的测量性能以及其他因素,例如校准的准确性和光学对准的稳定性。比较,分析和讨论了地面仪器的测量和模拟结果。通过使用附加的反向散射激光雷达验证了模拟的大气气溶胶模型。在高达17 km的高度上,测得的激光雷达原型的瑞利背向散射信号与模拟进行了比较,并显示出良好的一致性,相差2倍以上,包括对不同误差源的分析。首先分析了高卷云在Mie接收器处的信号。此外,将地面和飞机上的大气激光多普勒仪器(ALADIN)机载演示器(A2D)仪器的瑞利信号强度的仿真与卫星系统的仿真进行了比较。 11.5 km以上的卫星信号强度大于A2D地面仪器的信号强度,并且在所有高度下始终小于飞机的信号强度。

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  • 来源
    《Journal of atmospheric and oceanic technology》 |2009年第12期|2516-2530|共15页
  • 作者单位

    Deutsches Zentrum fuer Luft- und Raumfahrt, Institut fuer Physik der Atmosphaere, Oberpfaffenhofen, Germany;

    Deutsches Zentrum fuer Luft- und Raumfahrt, Institut fuer Physik der Atmosphaere, Oberpfaffenhofen, Germany;

    Deutsches Zentrum fuer Luft- und Raumfahrt, Institut fuer Physik der Atmosphaere, Oberpfaffenhofen, Germany;

    Deutsches Zentrum fuer Luft- und Raumfahrt, Institut fuer Physik der Atmosphaere, Oberpfaffenhofen, Germany;

    Physics Solutions, Munich, Germany;

    Ludwig-Maximilians-University of Munich, Munich, Germany;

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