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首页> 外文期刊>Journal of the Meteorological Society of Japan >Feasibility Study for Future Spaceborne Coherent Doppler Wind Lidar, Part 2: Measurement Simulation Algorithms and Retrieval Error Characterization
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Feasibility Study for Future Spaceborne Coherent Doppler Wind Lidar, Part 2: Measurement Simulation Algorithms and Retrieval Error Characterization

机译:未来航天飞机的可行性研究相干多普勒风潮,第2部分:测量仿真算法和检索误差表征

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A feasibility study of tropospheric wind measurements using a coherent Doppler lidar aboard a super low altitude satellite is being conducted in Japan. The considered lidar uses a 2.05 mu m laser light source of 3.75 W. In order to assess the measurement performances, simulations of wind measurements were conducted. The mission definition is presented in a companion paper (Part 1) while, in this paper, we describe the measurement simulator and characterize the errors on the retrieved line-of-sight (LOS) winds. Winds are retrieved from the Doppler-shift of the noisy backscattered signal with a horizontal resolution of 100 km along the orbit track and a vertical resolution between 0.5 and 2 km. Cloud and wind fields are the pseudo-truth of an Observing System Simulation Experiment while aerosol data are from the Model-of-Aerosol-Species-IN-the-Global-AtmospheRe (MASINGAR) constrained with the pseudo-truth wind. We present the results of the analysis of a full month of data in summer time for a near-polar orbiting satellite and a LOS nadir angle of 35 degrees. Below approximate to 8 km, the ratio of good retrievals is 30-55 % and the median LOS wind error is better than 0.6 m s(-1) (1.04 m s(-1) for the horizontal wind). In the upper troposphere, the ratio is less than 15 % in the southern hemisphere and high-latitudes. However, the ratio is still 35 % in the northern Tropics and mid-latitudes where ice-clouds frequently occur. The upper-tropospheric median LOS-wind measurement error is between 1-2 m s(-1) depending on the latitude (1.74-3.5 m s(-1) for the horizontal wind). These errors are dominated by uncertainties induced by spatial atmospheric inhomogeneities.
机译:使用连贯的多普勒LIDAR的对流层风测量的可行性研究在日本进行了超低海拔卫星。所考虑的激光雷达使用3.75W的2.05 mu m激光光源。为了评估测量性能,进行风测量的模拟。任务定义呈现在伴侣纸(第1部分)中,同时,在本文中,我们描述了测量模拟器,并表征了检索到的视线(LOS)风中的错误。从嘈杂的反向散射信号的多普勒转移检出风,沿轨道轨道的水平分辨率,横向分辨率,垂直分辨率在0.5到2公里之间。云和风田是观察系统仿真实验的伪真理,而气溶胶数据来自全球范围内的气溶胶型号(Masingar),受到伪真实风的限制。我们在夏季时间为近极轨道卫星和LOS Nadir角度提供了对夏季时间的全月份数据的分析结果。低于8km的近似,良好检索比率为30-55%,中位数洛斯风误差优于0.6米(-1)(水平风1.04 m s(-1))。在对流层的上层,南半球和高纬度的比例小于15%。然而,北热带地区的比例仍然是35%,以及经常发生冰云的中期纬度。上层中位数洛斯风测量误差在1-2 m S(-1)之间,取决于水平风的纬度(1.74-3.5 m s(-1))。这些误差是由空间大气不均匀诱导的不确定性的主导。

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