Calibration of the Instrumental Errors on Marine Gravity Recovery from SWOT Altimeter

大地测量学 海洋表面地形 大地水准面 高度计 遥感 校准 海面高度 地质学 重力异常 地球物理学 物理 实测深度 量子力学 古生物学 油田
作者
Gang Ma,Taoyong Jin,Jiang Pengyuan,Jiasheng Shi,Mao Zhou
出处
期刊:Marine Geodesy [Informa]
卷期号:46 (6): 496-522 被引量:5
标识
DOI:10.1080/01490419.2023.2232107
摘要

AbstractAbstractThe wide-swath altimetry mission, Surface Water and Ocean Topography (SWOT), makes it possible to further break through the accuracy and resolution of marine gravity field recovery. However, as its main payload, the Ka-band radar interferometer (KaRIN) is easy to be affected by the spacecraft attitude, mechanical deformations and dual antenna signal reception status, which generates instrumental errors including roll errors, phase errors, baseline dilation errors, timing errors, and KaRIN noise. Together with ocean temporal variations, the instrumental errors have large effects on the SWOT Sea Surface Height (SSH) observations and hence the marine gravity field recovery. Here, taking the sea area around Japan as an example, we investigated the calibrations of instrumental errors and ocean temporal variations on the recovery of the marine gravity field. The SSH observations of SWOT are first simulated by Mean Sea Surface (MSS), Absolute Dynamic Topography (ADT), Mean Dynamic Topography (MDT) and instrumental errors. Next, the influence of instrumental errors on determining vertical deflection within single-cycle data was analyzed. Then, three calibration methods (KaRIN/KaRIN cross-calibration, Representative KaRIN/KaRIN cross-calibration, and KaRIN/Nadir cross-calibration) are used to reduce the instrumental errors; the experimental results show KaRIN/KaRIN cross-calibration is the optimal one. Last, for the multi-cycle observations containing ocean temporal variations, crossover calibration is done in single cycle and then followed by collinear adjustment in multi-cycles. This approach is verified by considering 18 simulated cycles that cover almost 1 year. Our result indicates an improvement in the accuracy of marine gravity anomaly by about 45% compared to that of one cycle. The calibration strategy of instrumental errors and ocean temporal variations can be used for high-precision marine gravity field recovery with abundant SWOT observations in the near future.Keywords: Crossover calibrationinstrumental errorsmarine gravitySWOT altimetervertical deflection Disclosure statementNo potential conflict of interest was reported by the authors.Additional informationFundingThis study is supported by National Natural Science Foundation of China under Grants 41974020 and 42192533, and the Special Fund of Hubei Luojia Laboratory under Grant 220100001.
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