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首页> 外文期刊>Geophysical Research Letters >Airborne scanning lidar observations of aircraft contrails and cirrus clouds during SUCCESS
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Airborne scanning lidar observations of aircraft contrails and cirrus clouds during SUCCESS

机译:成功期间飞机上的转换轨迹和卷云的机载扫描激光雷达观测

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摘要

An angular scanning backscatter lidar was deployed on the NASA DC-8 research aircraft as part of SUCCESS. The lidar viewing direction could be continuously scanned from vertically upward to forward to vertically downward. Real-time pictorial displays generated from lidar signatures were used to locate clouds and contrails above, ahead of, and below the DC-8; to depict their spatial structure; and to help select DC-8 altitudes for achieving optimum sampling by onboard in situ sensors. The lidar data are being analyzed to establish their value in the interpretation and extension of the in situ sensor databases. Data examples are presented that illustrate (1) correlation with particulate, gas, and radiometric measurements made by onboard sensors, (2) discrimination and identification between contrails observed by the onboard sensors, (3) a 13.1 km altitude layer that exhibits greatly enhanced vertical backscatter relative to off-vertical backscatter, and (4) mapping of vertical distributions of individual precipitating ice crystals and their capture by cloud layers. [References: 8]
机译:作为成功的一部分,在美国国家航空航天局DC-8研究飞机上部署了角向扫描反向散射激光雷达。激光雷达的观察方向可以从垂直向上连续扫描到正向,然后再向下垂直扫描。由激光雷达信号生成的实时图形显示用于在DC-8上方,下方和下方定位云层和凝结尾迹;描绘其空间结构;并帮助选择DC-8高度,以通过车载原位传感器实现最佳采样。正在对激光雷达数据进行分析,以建立其在原位传感器数据库的解释和扩展中的价值。给出的数据示例说明了(1)与机载传感器进行的微粒,气体和辐射测量之间的相关性;(2)机载传感器观测到的凝结尾迹之间的区别和识别;(3)高度显着增强的13.1 km高度层相对于非垂直向后散射的反向散射,以及(4)单个降水冰晶的垂直分布及其被云层捕获的映射。 [参考:8]

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