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First shipborne GNSS-R campaign for receiving low elevation angle sea surface reflected signals

机译:首次接收低仰角海面反射信号的舰载GNSS-R运动

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Global Navigation Satellite System Reflectometry (GNSS-R) was regarded as a promising way to observe atmospheric duct by utilizing low elevation angle ocean surface reflected signals. To invest the Delay maps' feature of low elevation angle reflected signals in the atmospheric duct, a shipborne GNSS-R campaign was conducted in July, 2015 by the scientific investigation ship called Shiyan 3 on the South China Sea. During the campaign, the atmospheric temperature, pressure, and relative humidity which were used to detect atmospheric duct were recorded by GPS radiosondes and meteorological recorder. The GNSS-R payload developed by National Space Science Center (NSSC) and fixed on the rail of Shiyan3 was used to generate Delay maps. Preliminary results showed that atmospheric duct, especially evaporation duct, existed almost all the time in the experimental ocean region. Ocean surface reflected signals with elevation angle less than 10° were received and formed delay maps successfully. Affected by the direct signal and specular reflected signal's strong interference, apparent code correlation peaks appeared on Delay maps' tail. The experimental values of correlation peaks and simulated code autocorrelation were synthetically used to fit the curve of direct signal and specular reflected signal's strong interference utilizing the least square method. After removing the interference, cleaner reflected signals without direct and specular reflection signals were obtained.
机译:全球导航卫星系统反射法(GNSS-R)被认为是通过利用低仰角海面反射信号观测大气管道的一种有前途的方法。为研究大气导管中低仰角反射信号的延迟图特征,2015年7月,一艘名为“十堰3号”的科学考察船在南海进行了舰载GNSS-R运动。在竞选期间,用于探测大气管道的大气温度,压力和相对湿度由GPS无线电探空仪和气象记录仪记录。由国家空间科学中心(NSSC)开发并固定在十堰3轨道上的GNSS-R有效载荷用于生成延迟图。初步结果表明,大气大管,特别是蒸发管,几乎一直存在于实验海洋区域。接收到仰角小于10°的海面反射信号,并成功形成了延迟图。受直接信号和镜面反射信号的强烈干扰的影响,在延迟图的尾部出现了明显的代码相关峰。利用最小二乘法综合利用相关峰和模拟代码自相关的实验值拟合直射信号和镜面反射信号的强干扰曲线。消除干扰后,可以获得没有直接反射和镜面反射信号的较干净的反射信号。

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