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An improved GRACE monthly gravity field solution by modeling the non-conservative acceleration and attitude observation errors

机译:通过对非保守加速度和姿态观测误差进行建模,改进了GRACE月度重力场解决方案

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摘要

The main contribution of this study is to improve the GRACE gravity field solution by taking errors of non-conservative acceleration and attitude observations into account. Unlike previous studies, the errors of the attitude and non-conservative acceleration data, and gravity field parameters, as well as accelerometer biases are estimated by means of weighted least squares adjustment. Then we compute a new time series of monthly gravity field models complete to degree and order 60 covering the period Jan. 2003 to Dec. 2012 from the twin GRACE satellites' data. The derived GRACE solution (called Tongji-GRACE02) is compared in terms of geoid degree variances and temporal mass changes with the other GRACE solutions, namely CSR RL05, GFZ RL05a, and JPL RL05. The results show that (1) the global mass signals of Tongji-GRACE02 are generally consistent with those of CSR RL05, GFZ RL05a, and JPL RL05; (2) compared to CSR RL05, the noise of Tongji-GRACE02 is reduced by about 21 % over ocean when only using 300 km Gaussian smoothing, and 60 % or more over deserts (Australia, Kalahari, Karakum and Thar) without using Gaussian smoothing and decorrelation filtering; and (3) for all examples, the noise reductions are more significant than signal reductions, no matter whether smoothing and filtering are applied or not. The comparison with GLDAS data supports that the signals of Tongji-GRACE02 over St. Lawrence River basin are close to those from CSR RL05, GFZ RL05a and JPL RL05, while the GLDAS result shows the best agreement with the Tongji-GRACE02 result.
机译:这项研究的主要贡献是通过考虑非保守加速度和姿态观测的误差来改进GRACE重力场解决方案。与以前的研究不同,姿态和非保守加速度数据,重力场参数以及加速度计偏差的误差是通过加权最小二乘平差进行估算的。然后,我们从双GRACE卫星的数据中计算出一个新的时间序列月度重力场模型,其阶次为60,阶次为2003年1月至2012年12月。将得出的GRACE解决方案(称为Tongji-GRACE02)在大地水准面方差和时间质量变化方面与其他GRACE解决方案(即CSR RL05,GFZ RL05a和JPL RL05)进行了比较。结果表明:(1)同济-GRACE02的整体质量信号与CSR RL05,GFZ RL05a和JPL RL05的信号基本一致; (2)与CSR RL05相比,仅使用300 km高斯平滑,同济GRACE02的噪声在海洋上降低了约21%,而在不使用高斯平滑的情况下,在沙漠(澳大利亚,卡拉哈里,卡拉库姆和塔尔)上的噪声降低了60%以上和去相关过滤; (3)对于所有示例,无论是否应用平滑和滤波,降噪效果都比信号降低效果更为显着。与GLDAS数据的比较表明,圣劳伦斯河流域的同济-GRACE02信号与CSR RL05,GFZ RL05a和JPL RL05的信号接近,而GLDAS结果与同济-GRACE02结果显示出最好的一致性。

著录项

  • 来源
    《Journal of Geodesy》 |2016年第6期|503-523|共21页
  • 作者单位

    Tongji Univ, Coll Surveying & Geoinformat, Shanghai 200092, Peoples R China|Hong Kong Polytech Univ, Dept Land Surveying & Geoinformat, Hong Kong, Hong Kong, Peoples R China|Ctr Spatial Informat Sci & Sustainable Dev, Shanghai, Peoples R China;

    Tongji Univ, Coll Surveying & Geoinformat, Shanghai 200092, Peoples R China;

    Hong Kong Polytech Univ, Dept Land Surveying & Geoinformat, Hong Kong, Hong Kong, Peoples R China;

    Guangdong Univ Technol, Dept Surveying & Mapping, Guangzhou, Guangdong, Peoples R China;

    Chinese Acad Sci, Inst Geodesy & Geophys, State Key Lab Geodesy & Earths Dynam, Wuhan, Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Satellite geodesy; GRACE; Monthly gravity field model; Non-conservative acceleration;

    机译:卫星大地测量GRACE月重力场模型非保守加速度;
  • 入库时间 2022-08-18 03:40:55

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