4.7 Article

Observing Sea Surface Current by Gaofen-3 Satellite Along-Track Interferometric SAR Experimental Mode

Publisher

IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
DOI: 10.1109/JSTARS.2021.3099105

Keywords

Satellites; Sea surface; Spaceborne radar; Sea measurements; Current measurement; Synthetic aperture radar; Radar imaging; Along-track interferometric synthetic aperture radar (along-track InSAR; ATI); Gaofen-3 satellite; sea surface current

Funding

  1. National Natural Science Foundation of China Study on remote sensing mechanisms and low backscattering information extraction of Zhoushan upwelling by space-borne synthetic aperture radar [41976174]
  2. China High Resolution Earth Observation System Program [41-Y30F07-9001-20/22]

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Sea surface current is a research hotspot in oceanography, and the observation experiment in the Jiaozhou Gulf effectively utilized the Gaofen-3 satellite's ATI experimental mode. The data was preprocessed and the current was extracted based on the M4S mode, with comparison to ground-based high frequency surface wave radar data showing that the surface current observed by the GF-3 satellite had a root mean square error of less than 0.2 m/s.
Sea surface current is a research hotspot in oceanography. Space-borne along-track interferometric synthetic aperture radar (along-track InSAR, ATI) is a promising sensor for measuring high-resolution sea surface current field, and there is no operational system in orbit yet. To support future space-borne ATI systems, based on the ATI experimental mode of the Gaofen-3 (GF-3) satellite, the first sea surface current observing experiment was conducted in the Jiaozhou Gulf in China, in 2019. Meanwhile, SAR observations and in situ instrument measurements of the current are obtained in the experiments. The data is first preprocessed by a processor specially developed for the GF-3 ATI data. Then, the current is extracted based on the M4S mode. The retrieved current of the Jiaozhou Gulf is compared with ground-based high frequency surface wave radar data. The results show that the root mean square error of the surface current observed by the GF-3 satellite is less than 0.2 m/s.

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