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The Application of Sea Wave Slope Distribution Empirical Dependences in Estimation of Interaction Between Microwave Radiation and Rough Sea Surface

机译:海浪斜率分布经验相关性在估算微波辐射与海浪相互作用中的应用

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摘要

The use of hydrological (surface wind and sea wave slope) dependences for the calculation of microwave characteristics of the “ocean–atmosphere” system by Kirchhoff method is discussed here. As an important example, we review results of our experiment on bistatic sensing of the sea surface. In this experiment, Sun is a powerful natural source of noise microwave radiation for the sea surface sensing. For the receiving of solar radiation in the region of quasi-specular scattering, three two-polarization radiometers (0.8, 2.25, and 6.0 cm) are used. The results of joint hydrological and radiometric experiments (wind speed from 0 to 15 m/s) are reported. As a result, the improved quantitative model for microwave (3–50-GHz band) radiometric calculations in remote sensing of “ocean–atmosphere” system is presented.
机译:本文讨论了使用水文(地表风和海浪坡度)依赖性通过基尔霍夫方法计算“海洋-大气”系统的微波特性的方法。作为一个重要的例子,我们回顾了对海面的双基地传感的实验结果。在此实验中,太阳是用于海面传感的强大的自然噪声微波辐射源。为了接收准镜面散射区域中的太阳辐射,使用了三个两极化辐射计(0.8、2.25和6.0厘米)。报告了联合水文和辐射试验的结果(风速从0到15 m / s)。结果,提出了一种改进的定量模型,用于“海洋-大气”系统遥感中微波(3–50 GHz频带)辐射测量的计算。

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