Coherent marine radar mapping of ocean surface currents and directional wave spectra

D. Trizna
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引用次数: 2

Abstract

A coherent marine radar with 3-m resolution has been developed that measures the radial component of the orbital wave velocity of ocean waves, as well as the mean radial ocean surface velocity. This radar provides a direct measure of the ocean wave spectrum by means of 3D-FFT processing of a sequence of radial velocity images collected at a 0.8 Hz image rate. Typically, 512 images are used, covering periods of the order of ten minutes, allowing a modest number of wave groups to be measured. The mean radial velocity map is obtained by a superposition of all radial velocity images collected, allowing wave patterns to blend to the mean, resulting in a map of mean currents. A pair of such radars operated at a coastal site, separated by a few hundred meters along the coastline, could allow the combination of radial components to be combined into a mean current vector field. Results of an experiment run during the offshore passage of Hurricane Ida in 2009 are presented, collected at the U.S. Army Corps of Engineers Field Research Facility, Duck, N.C.
海洋表面流和定向波谱的相干海洋雷达制图
研制了一种分辨率为3米的相干海洋雷达,用于测量海浪轨道波速的径向分量和海面平均径向速度。该雷达通过3D-FFT处理以0.8 Hz图像速率收集的一系列径向速度图像,提供了对海浪频谱的直接测量。通常,使用512张图像,覆盖10分钟的周期,允许测量适度数量的波群。平均径向速度图是由收集到的所有径向速度图像的叠加得到的,允许波浪模式混合到平均值,从而得到平均洋流图。一对这样的雷达在沿海地区运行,沿着海岸线相隔几百米,可以将径向分量组合成平均电流矢量场。本文介绍了2009年飓风艾达近海通过期间进行的一项实验结果,这些结果收集于北卡罗来纳州达克市美国陆军工程兵团野外研究设施
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