坡度、波高和雷达光谱的比较,海上雷达散射的坡度和水动力调制

V. Hesany, R.K. Moore, S. Haimov
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引用次数: 2

摘要

对海浪的描述通常依赖于波高的点测量。海洋的重要矢量斜率通常必须从点测量和线性假设或从雷达足迹中无法得到的俯仰和横摇浮标中得出。我们开发了一种35 ghz矢量斜率计,采用单开关波束天线。它可以测量三个相邻的海洋高度剖面,从中我们可以得到两个正交的斜率分量。我们在1990年11月的SAXON-FFN实验中使用了矢量斜率计。同时测量长波斜率和后向散射功率的正交分量,可以确定斜率调制和bragg谐振纹波振幅的水动力调制对雷达信号总体调制的相对贡献。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Comparison of Slope, Wave Height, and Radar Spectra, Slope and Hydrodynamic Modulation of Radar Scatter from the Sea
Description of Ocean waves usually depends on point measurements of wave height. The important vector slope of the ocean must usually be derived either from point measurements and linear assumptions or from pitch-and-roll buoys that cannot be in the radar footprint. We developed a 35-GHz vector slope gaugehat- terometer using a single switched-beam antenna. It can measure three adjacent height profiles of the ocean, from which we can derive two orthogonal components of the slope. We used the vector slope gauge during the SAXON-FFN experiment in November, 1990. Simultaneous measurements of the orthogonal components of the long-wave slopes and the backscattered power permit determination of the relative contribution to the overall modulation of the radar signal by slope modulation and hydrody- namic modulation of Bragg-resonant ripple amplitude.
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