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AN INITIAL INVESTIGATION OF THE GOCE ERROR VARIANCE-COVARIANCE MATRICES IN THE CONTEXT OF THE GOCE USER TOOLBOX PROJECT

机译:探讨了Goce用户工具箱项目上下文中Goce错误方差 - 协方差矩阵的初步调查

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The availability of the full error variance-covariance matrices for the GOCE gravity field models is an important feature of the GOCE mission. Potentially, it will allow users to evaluate the accuracy of a geoid ormean dynamic topography (MDT) derived from the gravity field model at any particular location, design optimal filters to remove errors from the surfaces, and rigorously assimilate a geoid/MDT into ocean models, or otherwise combine the GOCE gravity field with other data. Here we present an initial investigation into the error characteristics of the GOCE gravity field models as they are realised in the calculated geoid anomalies. We examine how the error variances depend on location and spatial scale, and how they differ between models. The inhomogeneous and anisotropic nature of the error covariances are explored, and an example of how this information may be used in ocean data assimilation is provided. Finally, we consider some of the practical issues relating to the handling of the huge files containing the error variance-covariance information.
机译:Goce重力场模型的完整错误方差 - 协方差矩阵是衰减使命的重要特征。潜在地,它将允许用户评估从任何特定位置的Gravity场模型导出的大地形或MDT)的准确性,设计最佳过滤器以消除表面的误差,并严格同化到海洋模型的水流/ MDT ,或以其他方式将Goce重力场与其他数据组合。在这里,我们对Goce重力场模型的误差特性提出了初步调查,因为它们在计算出的大麻袋异常中实现。我们检查错误差异如何取决于位置和空间尺度,以及它们之间的模型之间的差异。探索了误差协方差的不均匀和各向异性的性质,提供了如何在海洋数据同化中使用该信息的示例。最后,我们考虑与处理包含错误方差 - 协方差信息的庞大文件有关的一些实际问题。

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