Influence of Radar Parameters and Sea State on Wind Wave-Induced Velocity in C-Band ATI SAR Ocean Surface Currents

Wind wave-induced artifact surface velocity (WASV) is an important component of the sea surface motions detected by synthetic aperture radar (SAR) systems. Understanding the characteristics of the interference of WASV on SAR current velocity estimates is necessary to improve the accuracy of retrieva...

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Main Authors: Rui Zhang, Jie Zhang, Xi Zhang, Chenghui Cao, Xiaochen Wang, Gui Gao, Genwang Liu, Meng Bao
Format: Article
Language:English
Published: MDPI AG 2022-08-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/14/17/4135
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author Rui Zhang
Jie Zhang
Xi Zhang
Chenghui Cao
Xiaochen Wang
Gui Gao
Genwang Liu
Meng Bao
author_facet Rui Zhang
Jie Zhang
Xi Zhang
Chenghui Cao
Xiaochen Wang
Gui Gao
Genwang Liu
Meng Bao
author_sort Rui Zhang
collection DOAJ
description Wind wave-induced artifact surface velocity (WASV) is an important component of the sea surface motions detected by synthetic aperture radar (SAR) systems. Understanding the characteristics of the interference of WASV on SAR current velocity estimates is necessary to improve the accuracy of retrievals. In this study, we assessed and analyzed the sensitivity of WASV in C-band along-track interferometric (ATI) SAR to radar configuration, wind field, swell field, and a wave spectrum model. Results showed that the influence of wind speed on WASV increased with the current velocity. The swell also affected WASV, especially at higher wind speeds; WASV was more strongly influenced by swell amplitude than by swell wavelength. In terms of radar configurations, results showed that VV polarization was more suitable than HH polarization in the estimation of WASV. The interference of WASV was minimal at moderate incidence angles (around 40°), and an appropriate ATI baseline selection was also given. The WASV was more strongly influenced by sea states than by the wave spectrum model or by a spreading function. The findings of this study improve our understanding of WASV and provide a reference for the design of future ATI SAR current measurement instruments and projects.
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spelling doaj.art-0012e431ef08446aacd6db2ee5393aed2023-11-23T14:01:28ZengMDPI AGRemote Sensing2072-42922022-08-011417413510.3390/rs14174135Influence of Radar Parameters and Sea State on Wind Wave-Induced Velocity in C-Band ATI SAR Ocean Surface CurrentsRui Zhang0Jie Zhang1Xi Zhang2Chenghui Cao3Xiaochen Wang4Gui Gao5Genwang Liu6Meng Bao7First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, ChinaFirst Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, ChinaFirst Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, ChinaFirst Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, ChinaKey Laboratory of Technology in Geo-Spatial Information Processing and Application Systems, Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100190, ChinaFaculty of Geosciences and Environmental Engineering, Southwest Jiaotong University, Chengdu 611756, ChinaFirst Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, ChinaFirst Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, ChinaWind wave-induced artifact surface velocity (WASV) is an important component of the sea surface motions detected by synthetic aperture radar (SAR) systems. Understanding the characteristics of the interference of WASV on SAR current velocity estimates is necessary to improve the accuracy of retrievals. In this study, we assessed and analyzed the sensitivity of WASV in C-band along-track interferometric (ATI) SAR to radar configuration, wind field, swell field, and a wave spectrum model. Results showed that the influence of wind speed on WASV increased with the current velocity. The swell also affected WASV, especially at higher wind speeds; WASV was more strongly influenced by swell amplitude than by swell wavelength. In terms of radar configurations, results showed that VV polarization was more suitable than HH polarization in the estimation of WASV. The interference of WASV was minimal at moderate incidence angles (around 40°), and an appropriate ATI baseline selection was also given. The WASV was more strongly influenced by sea states than by the wave spectrum model or by a spreading function. The findings of this study improve our understanding of WASV and provide a reference for the design of future ATI SAR current measurement instruments and projects.https://www.mdpi.com/2072-4292/14/17/4135sea surface currentsynthetic aperture radar (SAR)along-track interferometry (ATI)C-bandwind wave-induced artifact surface velocity (WASV)simulation
spellingShingle Rui Zhang
Jie Zhang
Xi Zhang
Chenghui Cao
Xiaochen Wang
Gui Gao
Genwang Liu
Meng Bao
Influence of Radar Parameters and Sea State on Wind Wave-Induced Velocity in C-Band ATI SAR Ocean Surface Currents
Remote Sensing
sea surface current
synthetic aperture radar (SAR)
along-track interferometry (ATI)
C-band
wind wave-induced artifact surface velocity (WASV)
simulation
title Influence of Radar Parameters and Sea State on Wind Wave-Induced Velocity in C-Band ATI SAR Ocean Surface Currents
title_full Influence of Radar Parameters and Sea State on Wind Wave-Induced Velocity in C-Band ATI SAR Ocean Surface Currents
title_fullStr Influence of Radar Parameters and Sea State on Wind Wave-Induced Velocity in C-Band ATI SAR Ocean Surface Currents
title_full_unstemmed Influence of Radar Parameters and Sea State on Wind Wave-Induced Velocity in C-Band ATI SAR Ocean Surface Currents
title_short Influence of Radar Parameters and Sea State on Wind Wave-Induced Velocity in C-Band ATI SAR Ocean Surface Currents
title_sort influence of radar parameters and sea state on wind wave induced velocity in c band ati sar ocean surface currents
topic sea surface current
synthetic aperture radar (SAR)
along-track interferometry (ATI)
C-band
wind wave-induced artifact surface velocity (WASV)
simulation
url https://www.mdpi.com/2072-4292/14/17/4135
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