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首页> 外文期刊>IEEE Transactions on Geoscience and Remote Sensing >Assessment of Spaceborne GNSS-R Ocean Altimetry Performance Using CYGNSS Mission Raw Data
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Assessment of Spaceborne GNSS-R Ocean Altimetry Performance Using CYGNSS Mission Raw Data

机译:使用Cygnss Mission RAW数据评估Spaloborne GNSS-R海洋高度算法

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This article assesses the ocean altimetry performance of spaceborne Global Navigation Satellite Systems reflectometry (GNSS-R) by processing the raw data sets collected by the Cyclone GNSS (CYGNSS) constellation. These raw data sets, i.e., the intermediate frequency signal streams before any receiver processing, are processed on the ground with a software receiver, from which the reflected waveforms of GPS L1, Galileo E1, and BeiDou-3 B1 band open service (OS) signals are generated following the conventional GNSS-R approach. By using different retracking algorithms, the bistatic delays of the reflected signals are derived from these waveforms, in which the retracking biases are removed with the specular point (SP) delay and power information computed from the corresponding waveform model. After applying a set of standard delay corrections, the bistatic delay observations are converted into sea surface height (SSH) measurements and compared with the mean SSH model. Both the random error (precision) and systematic effects (accuracy) are characterized with intratrack and intertrack analyses of the bistatic delay measurements. The two-way ranging precision can reach up to 3.9 and 2.5 m with 1-s GPS and Galileo group delay measurement (a factor of 2 better for altimetry solution), and its evolution with the signal-to-noise ratio shows good consistency with the theoretical model. A significant delay dispersion of 3.0 m between different tracks is found, which is mainly attributed to the receiver orbit error and ionospheric correction residuals. These results can provide useful inputs for the development of future GNSS-R missions dedicated to ocean altimetry applications.
机译:本文通过处理由旋风GNSS(CYGNSS)星座收集的原始数据集来评估星球全球导航卫星系统反射仪(GNSS-R)的海洋高度性能。这些原始数据集,即,在任何接收器处理之前的中频信号流,在地面上处理,软件接收器,GPS L1,Galileo E1和Beidou-3 B1频带开放服务(OS)的反射波形。通过传统的GNSS-R方法产生信号。通过使用不同的传记算法,反射信号的双向延迟源自这些波形,其中通过镜面(SP)延迟和从相应的波形模型计算的电力信息去除所述回想偏置。在施加一组标准延迟校正之后,双静电延迟观察被转换为海表面高度(SSH)测量并与平均SSH模型进行比较。随机误差(精度)和系统效果(精度)都具有双腹部延迟测量的intertrack和Intertrack分析。双向测距可以达到3.9和2.5米,具有1-S GPS和伽利略组延迟测量(用于高处溶液的倍数2),其发出信噪比的演变显示出良好的一致性理论模型。找到不同轨道之间3.0米的显着延迟分散,主要归因于接收器轨道误差和电离层校正残余物。这些结果可以为未来GNSS-R任务的开发提供有用的投入,致力于海洋Altimetry应用程序。

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