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Remote sensing of ocean, ice and land surfaces using bistatically reflected GNSS signals from low Earth orbit

机译:使用来自低地球轨道的双基地反射GNSS信号遥感海洋,冰和陆地表面

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The reflection of (Global Navigation Satellites) signals from the Earth's surface has progressed to demonstrate a practical linkage of measurements to geophysical description of ocean, ice and land areas. Since launch of the small constellation, it has been successfully used to target and detect specular reflections of GPS signals after scattering from the Earth's oceans, ice sheets and land surfaces. All data sets have exposed reflected signals, including signals reflected off the ocean under different ocean conditions. This reveals that GNSS Reflectometry is a suitable future technology for space based Earth remote sensing, even when deployed on the UK DMC low Earth orbiting satellite system. This paper presents a summary of the signals collected from over the ocean, and an examination of the signal relationship to the ocean wind and wave conditions is presented. The initial results from ice and land surfaces reflection analysis are also described.
机译:来自地球表面的(全球导航卫星)信号的反射已经取得进展,证明了测量与海洋,冰和陆地区域的地球物理描述之间的实际联系。自从发射小型星座以来,它已经成功地用于定位和检测GPS信号在从地球海洋,冰原和陆地表面散射后的镜面反射。所有数据集都暴露了反射信号,包括在不同海洋条件下从海洋反射的信号。这表明,即使将其部署在英国DMC低地球轨道卫星系统上,GNSS反射法也是未来适用于基于空间的地球遥感的技术。本文概述了从海洋上收集到的信号,并对信号与海洋风浪条件之间的关系进行了研究。还描述了冰和陆地表面反射分析的初步结果。

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