利用水面反射的全球导航卫星系统信号确定大地水准面高度剖面和垂直线偏差的结果

V. Lopatin, M. Murzabekov, D.S. Bobrov
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引用次数: 0

摘要

利用水面反射的全球导航卫星系统信号确定大地水准面高程的方法称为双稳态法。其特点是必要的机载设备体积小、重量轻,可以安装在一颗纳卫星上,同时确定几十个大地水准面高度剖面。它与全球轨道导航卫星系统、全球定位系统、伽利略系统、北斗系统中可见的导航卫星数量相当。国外实施了几个使用所述技术的空间项目,其分析表明有可能确定误差为 10-20 厘米的大地水准面高度以及海冰厚度。作者回顾了一些类似项目,评估了同时确定的大地水准面高度剖面数,并根据 CYGNSS 项目的主要测量数据计算了其高程和沿单一剖面的垂直偏转。在计算大地水准面高程时,为了补偿各种干扰参数,使用了以下模型
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Results of determining the geoid height profile and vertical line deviation using GNSS signals reflected from water surface
The method for determining geoid elevations, based on the use of GNSS signals reflected from water surface, is called bistatic one. Its features are small dimensions and weight of the necessary on-board equipment, and that enables mounting them on a nano-satellite, as well as simultaneously determining several dozen geoid height profiles. It corresponds to the number of visible navigation satellites from among GLONASS, GPS, Galileo, BeiDou. Several space projects using the technology under description were implemented abroad, their analysis has shown the possibility of determining geoid heights with an error of 10–20 cm, as well as sea ice thickness. The authors provide a review of some similar projects, an assessment of the simultaneously determined number of geoid height profiles, and calculation of its elevations and deflection of vertical along a single profile based on primary measurements from the project of CYGNSS. To compensate for various interfering parameters when calculating geoid elevations, the following models were used
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