利用来自近地轨道的双静态反射GNSS信号对海洋、冰和陆地表面进行遥感

Jabir Shabbir Malik, U. I. Bhatti
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引用次数: 10

摘要

从地球表面反射(全球导航卫星)信号已经取得进展,显示出测量与海洋、冰和陆地地区的地球物理描述之间的实际联系。自从这个小星座发射以来,它已经成功地用于定位和探测从地球海洋、冰盖和陆地表面散射的GPS信号的镜面反射。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,即使部署在英国DMC低地球轨道卫星系统上,GNSS反射计也是一种适合未来空间地球遥感的技术。本文概述了从海洋上空收集到的信号,并对信号与海洋风浪条件的关系进行了研究。本文还介绍了冰面和陆面反射分析的初步结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Remote sensing of ocean, ice and land surfaces using bistatically reflected GNSS signals from low Earth orbit
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.
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