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一种用于海洋观测的接收端相干X波段船用雷达。

A Coherent on Receive X-Band Marine Radar for Ocean Observations.

作者信息

Horstmann Jochen, Bödewadt Jan, Carrasco Ruben, Cysewski Marius, Seemann Jörg, Streβer Michael

机构信息

Helmholtz-Zentrum Hereon, Max Planck Str.1, 21502 Geesthacht, Germany.

出版信息

Sensors (Basel). 2021 Nov 25;21(23):7828. doi: 10.3390/s21237828.

Abstract

Marine radars are increasingly popular for monitoring meteorological and oceanographic parameters such as ocean surface wind, waves and currents as well as bathymetry and shorelines. Within this paper a coherent on receive marine radar is introduced, which is based on an incoherent off the shelf pulsed X-band radar. The main concept of the coherentization is based on the coherent on receive principle, where the coherence is achieved by measuring the phase of the transmitted pulse from a leak in the radar circulator, which then serves as a reference phase for the transmitted pulse. The Doppler shift frequency can be computed from two consecutive pulse-pairs in the time domain or from the first moment of the Doppler spectrum inferred by means of a short time Fast Fourier Transform. From the Doppler shift frequencies, radial speed maps of the backscatter of the ocean surface are retrieved. The resulting backscatter intensity and Doppler speed maps are presented for horizontal as well as vertical polarization, and discussed with respect to meteorological and oceanographic applications.

摘要

船用雷达在监测气象和海洋学参数(如海面风、海浪和海流以及测深和海岸线)方面越来越受欢迎。本文介绍了一种基于非相干现成脉冲X波段雷达的接收端相干船用雷达。相干化的主要概念基于接收端相干原理,即通过测量雷达环行器泄漏的发射脉冲的相位来实现相干,该相位随后用作发射脉冲的参考相位。多普勒频移可以在时域中从两个连续的脉冲对计算得出,也可以通过短时快速傅里叶变换从推断出的多普勒频谱的一阶矩计算得出。根据多普勒频移,可以获取海面后向散射的径向速度图。给出了水平和垂直极化情况下的后向散射强度和多普勒速度图,并针对气象和海洋学应用进行了讨论。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6eea/8659718/903901f837d1/sensors-21-07828-g001.jpg

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