Measurements of the Sea Surface Waves Parameters and the Doppler Spectrum of the Reflected Signal Using Optical and Acoustic Remote Sensing Methods

M. Ryabkova, V. Titov, Yu. L. Titchenko, E. Meshkov, V. Karaev, A. Yablokov, K. Ponur, R. Belyaev, M. Panfilova
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Abstract

Active and passive remote sensing techniques can be used simultaneously and their results complete each other. This paper introduces the results of the experiment that took place in October 2019 on the offshore platform in the Black Sea. Two unique pieces of equipment developed in the Institute of Applied Physics were used in the experiment: set of original optical devices for recording of range - time - intensity (RTI) images of sea surface and an underwater acoustic wave gauge. The devices were installed close to each other, optical devices were measuring slope spectrum, acoustic wave gauge can measure significant wave height and variance of slopes of the large-scale (in comparison with the wavelength of the incidence acoustic wave) waves, also the Doppler spectrum of the reflected signal can be measured. The string wave gauge is working on the platform constantly and provides measurements of the omnidirectional spectrum.
用光学和声学遥感方法测量海面波参数和反射信号的多普勒频谱
主动和被动遥感技术可以同时使用,其结果可以相互补充。本文介绍了2019年10月在黑海海上平台上进行的实验结果。实验使用了应用物理研究所研制的两套独特的设备:一套用于记录海面距离-时间-强度(RTI)图像的原始光学装置和一套水声波计。装置相互靠近安装,光学装置测量斜率谱,声波计可以测量大尺度(与入射声波波长相比)波的显著波高和斜率方差,还可以测量反射信号的多普勒频谱。管柱测波仪在平台上持续工作,提供全向频谱测量。
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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