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On weighted total least-squares for geodetic transformations

机译:大地变换的加权总最小二乘

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In this contribution, it is proved that the weighted total least-squares (WTLS) approach preserves the structure of the coefficient matrix in errors-in-variables (EIV) model when based on the perfect description of the dispersion matrix. To achieve this goal, first a proper algorithm for WTLS is developed since the quite recent analytical solution for WTLS by Schqffrin and Wieser is restricted to the condition Pa = (P_0(⊕) P_x) (where (⊕) is used to denote the Kronecker product) for the weight matrix of the coefficient matrix in the EIV model. This situation can be seen in the case of an affine transformation where the univariate approach can be an appropriate alternative to the multivariate WTLS approach, which has been applied to the affine transformation by Schaffrin and Felus, resp. Schaffrin and Wieser with restrictions similar to P_a = (P_0 (⊕) P_x)- In addition, this algorithm for WTLS can be interpreted well in the geodetic literature since it is based on the perfect description of the inverse dispersion matrix (or variance-covariance). By using the algorithm of WTLS, one obtains more realistic results in some applications of transformation where a high precision is needed. Some empirical examples, resp. simulation studies give insight into the efficiency of the procedure.
机译:在此贡献中,证明了当基于色散矩阵的完美描述时,加权总最小二乘(WTLS)方法在变量误差(EIV)模型中保留了系数矩阵的结构。为了实现此目标,首先开发了一种适用于WTLS的算法,因为Schqffrin和Wieser的WTLS的最新解析解决方案仅限于条件Pa =(P_0(⊕)P_x)(其中(⊕)表示克罗内克EIV模型中系数矩阵的权重矩阵)。在仿射变换的情况下可以看到这种情况,其中单变量方法可以替代多变量WTLS方法,后者已由Schaffrin和Felus分别应用于仿射变换。 Schaffrin和Wieser的限制类似于P_a =(P_0(P)P_x)-此外,该WTLS算法可以在大地测量文献中很好地解释,因为它基于对逆色散矩阵(或方差-协方差)的完美描述)。通过使用WTLS算法,在需要高精度的某些转换应用中可以获得更现实的结果。一些经验的例子,分别。仿真研究可以深入了解该过程的效率。

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