Abstract
The case of a singular dispersion matrix within the Gauss–Helmert Model has been considered before, most recently even allowing the rank of BQ to be smaller than the rank of B. In this contribution the emphasis is shifted towards an illuminating example, the 2D Helmert transformation.
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Acknowledgments
The first author would like to gratefully acknowledge the support of a Feodor-Lynen Research Fellowship from the Alexander-von-Humboldt Foundation (Germany), and the School of Earth Sciences at the Ohio State University (Columbus/OH, USA), with Prof. Schaffrin as his host. This manuscript was actually completed when the second author visited Prof. Neitzel, again with funds of the AvH-Foundation, which is also gratefully acknowledged.
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Appendix
Appendix
Estimated dispersion matrix of the estimated parameters \( \hat{\xi }_{0} ,\;\hat{\xi }_{1} ,\;\hat{\xi }_{2} ,\;\hat{\xi }_{3} , \) respectively for \( \hat{\omega } \) and \( \hat{\alpha }, \) from inverting (2.3), including their covariances, for the numerical example:
Estimated dispersion matrices for the residuals and their cross-covariance matrix:
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Neitzel, F., Schaffrin, B. Adjusting a 2D Helmert transformation within a Gauss–Helmert Model with a singular dispersion matrix where BQ is of smaller rank than B . Acta Geod Geophys 52, 479–496 (2017). https://doi.org/10.1007/s40328-016-0184-2
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DOI: https://doi.org/10.1007/s40328-016-0184-2