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Monitoring the performance of HY-2B and Jason-2/3 sea surface height via the China Altimetry Calibration Cooperation Plan

Yang Lei, Xu Yongsheng, Lin Mingsen, Ma Chaofei, Mertikas Stylianos, Hu Wei, Wang Zhiyong, Mu Bo, Zhou Xinghua

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URI: http://purl.tuc.gr/dl/dias/30624078-FC12-4C79-BBB2-DB793D7D271B
Year 2022
Type of Item Peer-Reviewed Journal Publication
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Bibliographic Citation L. Yang, Y. Xu, M. Lin, C. Ma, S. P. Mertikas, W. Hu, Z. Wang, B. Mu, and X. Zhou, "Monitoring the performance of HY-2B and Jason-2/3 sea surface height via the China Altimetry Calibration Cooperation Plan," IEEE Trans. Geosci. Remote Sens., vol. 60, 2022, doi: 10.1109/TGRS.2022.3153631. https://doi.org/10.1109/TGRS.2022.3153631
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Summary

Calibration and validation (Cal/Val) of the sea surface height as measured by satellite radar altimeters is essential to understand altimeter biases, observation trends, and instrument aging. It also supports the long-term stability of the produced climate change records of sea level as determined by altimetry. In this article, we report the calibration of HY-2B and Jason-2/3 using the established research infrastructure and data sharing initiative introduced by the Altimetry Calibration Cooperation Plan (ACCP) of China. Currently, three ACCP calibration sites encompass the Wanshan Islands, and two national oceanic sites are located along the China coastline. For each Cal/Val site, the components of the facilities—the geodetic, sea level, and Global Navigation Satellite System (GNSS) infrastructure—and the followed monitoring procedures and calibration methods are described. The HY-2B performance was primarily evaluated using about two years data, which indicated a mean bias of −0.2 ± 4.2 cm. Confidence in the results is strong, because the HY-2B biases were cross compared and confirmed by all the three independent sites and the three satellite ground tracks. Compared with its predecessor HY-2A, HY-2B shows very stable observations with no linear drift at present. In addition, Jason-2 and Jason-3 were mainly assessed using Qianliyan site. Our results indicate that the Jason-3 sea-surface height bias is approximately 2–3 cm smaller than that of Jason-2 and that the long-term stability of Jason-2/3 shows no significant trend, which in good agreement with the international dedicated sites. The instrument noises of Jason-2/3 and HY-2B were estimated based on the ACCP sites. The results show that the instrument noise in the previous literature is underestimated. This was also consolidated by the result from wavenumber spectrum and global crossover point analysis. The code and Wanshan data used in these Cal/Val experiments are publicly available to facilitate further work in this domain ( https://github.com/GenericAltimetryTools/CalAlti ).

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