不考虑小坡度和小高度假设的海面单散射雷达横截面

IF 1.5 4区 地球科学 Q3 ASTRONOMY & ASTROPHYSICS
Radio Science Pub Date : 2025-07-01 DOI:10.1029/2025RS008265
M. Torabi;R. Shahidi;E. W. Gill
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引用次数: 0

摘要

本文对高导电性随机表面的一阶雷达截面(RCS)进行了新的分析,特别关注了具有大粗糙度尺度和高频波段不可忽略斜率的海洋表面。采用广义函数方法,推导了控制海洋表面电场的算子方程。在先前研究的基础上,结合垂直脉冲偶极子源,我们的方法也解释了海洋表面的时变性质。通过在散射场表达式中引入显式的高度和表面坡度因子,我们得到了一个改进的一阶双基地RCS公式。这种方法减轻了传统的基于扰动的方法固有的限制,特别是在极端波浪条件下,从而提高了解释海洋表面遥感数据的潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Single-scattering radar cross section of the ocean surface without the small-slope and height assumptions
This paper presents a new analysis of the first-order radar cross section (RCS) of highly conductive random surfaces, with a particular focus on the ocean surface characterized by large roughness scales and non-negligible slopes in the high-frequency band. Employing a generalized-function approach, we derive the operator equation governing the electric field over the ocean surface. Building upon previous research and incorporating a vertical-pulsed dipole source, our methodology also accounts for the time-varying nature of ocean surfaces. By introducing explicit factors for height and surface slope into the scattering field expressions, we obtain an enhanced first-order bistatic RCS formulation. This approach alleviates restrictions inherent in traditional perturbation-based methods, particularly under extreme wave conditions, and thus offers improved potential for interpreting remote sensing data of the ocean surface.
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来源期刊
Radio Science
Radio Science 工程技术-地球化学与地球物理
CiteScore
3.30
自引率
12.50%
发文量
112
审稿时长
1 months
期刊介绍: Radio Science (RDS) publishes original scientific contributions on radio-frequency electromagnetic-propagation and its applications. Contributions covering measurement, modelling, prediction and forecasting techniques pertinent to fields and waves - including antennas, signals and systems, the terrestrial and space environment and radio propagation problems in radio astronomy - are welcome. Contributions may address propagation through, interaction with, and remote sensing of structures, geophysical media, plasmas, and materials, as well as the application of radio frequency electromagnetic techniques to remote sensing of the Earth and other bodies in the solar system.
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