雷达波束在大气湍流中的到达角

Proceedings of the 2002 IEEE Radar Conference (IEEE Cat. No.02CH37322) Pub Date : 2002-08-07 DOI:10.1109/NRC.2002.999728

R. McMillan, R. Smith, M. Shipman, E. J. Holder, J. C. Kerce, J. Williams

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引用次数: 8

摘要

大气湍流已被证明对雷达波束的到达角(AOA)有可测量的影响，但这些影响在几个微度的量级上，这对大多数应用来说是一个可以忽略不计的水平。在本文中，我们提出了一种描述这种现象的理论，并将该理论与使用x波段干涉雷达在3.5公里路径上进行的单向测量和在25公里路径上进行的双向测量进行比较。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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Angle-of-arrival of a radar beam in atmospheric turbulence

Atmospheric turbulence has been shown to have measurable effects on the angle-of-arrival (AOA) of radar beams, but these effects are on the order of a few microradians, which is a negligible level for most applications. In this paper, we present a theory describing this phenomenon and compare this theory to one-way measurements made over a 3.5 km path and two-way measurements made over a 25 km path using an X-band interferometric radar.

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Proceedings of the 2002 IEEE Radar Conference (IEEE Cat. No.02CH37322)

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