Evolution of high spatial resolution spaceborne scatterometers

R.A. Brown, R. Roeder
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引用次数: 2

Abstract

Satellite scatterometer (microwave radar) normalized radar backscatter measurements (/spl sigma//sup 0/) can be used to infer near-surface ocean wind speed and direction. The feasibility of scatterometer wind speed remote sensing was first proven with RADSCAT on SKYLAB in 1973. The technique was refined with the Seasat scatterometer in 1978 and work in the early 1990s by European and US space agencies has provided the foundation for continuous, global wind vector measurements. This paper discusses the need for improved scatterometer spatial resolution and the design evolution for planned future high resolution spaceborne scatterometers.
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高空间分辨率星载散射计的发展
卫星散射计(微波雷达)归一化雷达后向散射测量值(/spl sigma//sup 0/)可用于推断近地表海洋风速和风向。散射计风速遥感的可行性在1973年由SKYLAB的RADSCAT首次证实。这项技术在1978年与Seasat散射计一起得到改进,欧洲和美国空间机构在20世纪90年代初的工作为连续的全球风矢量测量提供了基础。本文讨论了提高散射计空间分辨率的需求和未来高分辨率星载散射计的设计演变。
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