北斗GEO卫星GNSS-R延迟信号功率波形分析

Mohammad Shohidul Islam, Dong-Kai Yang, Muhammad Abdul Alim Sikder
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引用次数: 0

摘要

GNSS遥感可以在地球表面监测中发挥重要作用。为此,提出了一种从水面提取信息的方法。具体来说,海面散射信号可以提供重要的海面信息和当前状况。本文主要对北斗GEO卫星的直接功率波形和散射功率波形进行了研究和分析。由于反射信号的延迟,其波形模式和特征与直接信号明显不同。这些功率波形是在不同的相干积分时间、不同的风速和不同的卫星仰角下确定的。利用Z-V散射模型和Tanos Elfouhaily波谱模型给出了反射信号的功率波形,并将这些波形与实际数据的反射和直接信号的功率波形进行了比较。结果表明,这些波形对积分时间、风速和卫星仰角都很敏感。研究还发现,波形与时间、风速和仰角这三个参数直接相关。结果表明,模型波形与实际数据波形吻合良好。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Power waveforms analysis of GNSS-R delay signals from beidou GEO satellite
GNSS remote sensing can play an important rule for monitoring the earth's surface. For this why, this technique is proposed to retrieve some information from water surface. Specifically, scattered signals from the ocean surface can provide significant information of water surface and its current condition. In this paper, direct and scattered power waveforms of GEO Satellite of Beidou are mainly focused and analyzed. Due to delay of reflected signal, the waveforms pattern & characteristics are clearly different from direct signals. These power waveforms are determined for different coherent integration times, different wind speeds and different satellite elevation angles. Z-V scattering model and Tanos Elfouhaily wave spectrum model are utilized to present the power waveforms of reflected signals and these waveforms are compared with the power waveforms of reflected & direct signals of real data. It is observed that these waveforms are sensitive to integration time, wind speed and satellite elevation angle. It is also found that the waveforms are directly related to these three parameters (time, wind speed & elevation angle). As a result, the model waveforms and real data waveforms have performed a good matching each other.
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