SWOT高度计海洋重力恢复仪器误差的校正

IF 2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Gang Ma, T. Jin, Pengyuan Jiang, Jiasheng Shi, Mao Zhou
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引用次数: 0

摘要

摘要广域测高任务,地表水和海洋地形(SWOT),使进一步突破海洋重力场恢复的准确性和分辨率成为可能。然而,Ka波段雷达干涉仪作为其主要有效载荷,容易受到航天器姿态、机械变形和双天线信号接收状态的影响,从而产生仪器误差,包括滚转误差、相位误差、基线膨胀误差、定时误差和KaRIN噪声。仪器误差与海洋时间变化一起,对SWOT海面高度(SSH)观测结果以及海洋重力场恢复产生了很大影响。本文以日本周边海域为例,研究了仪器误差和海洋时间变化对海洋重力场恢复的影响。SWOT的SSH观测首先通过平均海面(MSS)、绝对动态地形(ADT)、平均动态地形(MDT)和仪器误差进行模拟。其次,分析了仪器误差对单周数据内垂直挠度测定的影响。然后,使用三种校准方法(KaRIN/KaRIN交叉校准、代表性KaRIN/KaRIN交叉校准和KaRIN/Nadir交叉校准)来减少仪器误差;实验结果表明,KaRIN/KaRIN交叉校准是最佳的交叉校准。最后,对于包含海洋时间变化的多周期观测,在单周期内进行交叉校准,然后在多周期内进行共线平差。该方法通过考虑18个模拟循环来验证,这些模拟循环几乎涵盖了1 年我们的结果表明,与一个周期相比,海洋重力异常的精度提高了约45%。仪器误差和海洋时间变化的校准策略可以在不久的将来用于具有丰富SWOT观测的高精度海洋重力场恢复。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Calibration of the Instrumental Errors on Marine Gravity Recovery from SWOT Altimeter
Abstract The 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.
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来源期刊
Marine Geodesy
Marine Geodesy 地学-地球化学与地球物理
CiteScore
4.10
自引率
6.20%
发文量
27
审稿时长
>12 weeks
期刊介绍: The aim of Marine Geodesy is to stimulate progress in ocean surveys, mapping, and remote sensing by promoting problem-oriented research in the marine and coastal environment. The journal will consider articles on the following topics: topography and mapping; satellite altimetry; bathymetry; positioning; precise navigation; boundary demarcation and determination; tsunamis; plate/tectonics; geoid determination; hydrographic and oceanographic observations; acoustics and space instrumentation; ground truth; system calibration and validation; geographic information systems.
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