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GNSS-R Ocean Altitude Detection Technology Based on Carrier Phase Assistant

机译:基于载波相位助手的GNSS-R海洋高度检测技术

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GNSS-R is a new branch of GNSS which has been developed since the 1990s. It can be applied to remote sensing exploration of marine environment and remote sensing of terrestrial environment. GNSS-R has many advantages over other remote sensing techniques, such as remote sensing, Low cost, low power consumption, high spatial and temporal resolution, and many other advantages of the project can be detected. GNSS-R marine remote sensing detection technology mainly through high-gain reflection antenna to receive the GNSS reflection signal from the sea to complete the marine environmental detection, the reflected signal carries changes in signal waveforms, changes in polarization characteristics, amplitude, phase, and frequency. In this paper, a GNSS-R ocean height detection technique based on carrier phase assistant was introduced. The conventional channel accomplishes the initial acquisition of the signal and outputs the original DDM pattern by the time delay-Doppler mapping correlator, DDM diagram can be used to complete the inversion of the wind field, etc., while the DDM map contains the reflected signal doppler, time delay information, the accuracy of doppler and time delay was determined by the DDM Doppler interval and the time interval. The processor can process the time delay of the reflected signal to obtain a roughly phase and doppler information. The closed-loop acquisition and tracking of the signal was completed by the time information and doppler information obtained by the reflection. By calculating the direct and reflection channel carrier phase, pseudo-range difference for the sea surface height inversion. In order to verify the inversion accuracy of the system, in this paper, the ground-based test and flight test was carried out using the self-research phased-array GNSS-R ocean reflection receiver system. The experimental data showed that the inversion error of sea surface height was better than 10 cm.
机译:GNSS-R是GNSS的一个新分支,自1990年代以来就开始开发。它可以应用于海洋环境的遥感勘探和陆地环境的遥感。 GNSS-R与其他遥感技术相比具有许多优势,例如遥感,低成本,低功耗,高空间和时间分辨率,并且可以检测到该项目的许多其他优势。 GNSS-R海洋遥感探测技术主要通过高增益反射天线接收来自海上的GNSS反射信号来完成海洋环境检测,反射后的信号携带信号波形的变化,偏振特性,幅度,相位和幅度的变化。频率。本文介绍了一种基于载波相位辅助的GNSS-R海洋高度检测技术。常规通道完成了信号的初始捕获,并通过时延多普勒映射相关器输出了原始DDM模式,DDM图可用于完成风场的反演等,而DDM图则包含反射信号多普勒,时间延迟信息,多普勒的准确性和时间延迟由DDM多普勒间隔和时间间隔确定。处理器可以处理反射信号的时间延迟,以获得大致的相位和多普勒信息。信号的闭环采集和跟踪通过反射获得的时间信息和多普勒信息完成。通过计算直接和反射通道的载波相位,伪距差为海面高度反演。为了验证该系统的反演精度,本文采用自研究相控阵GNSS-R海洋反射接收机系统进行了地面试验和飞行试验。实验数据表明,海面高度反演误差优于10 cm。

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