4.4 Article

Use of the Comprehensive Inversion method for Swarm satellite data analysis

Journal

EARTH PLANETS AND SPACE
Volume 65, Issue 11, Pages 1201-1222

Publisher

SPRINGER
DOI: 10.5047/eps.2013.09.007

Keywords

Swarm; Earth's magnetic field; comprehensive modeling; core; lithosphere; ionosphere; magnetosphere; electromagnetic induction

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An advanced algorithm, known as the Comprehensive Inversion (CI), is presented for the analysis of Swarm measurements to generate a consistent set of Level-2 data products to be delivered by the Swarm Satellite Constellation Application and Research Facility (SCARF) to the European Space Agency (ESA). This new algorithm improves on a previously developed version in several ways, including the ability to process ground-based observatory data, estimation of rotations describing the alignment of vector magnetometer measurements with a known reference system, and the inclusion of ionospheric induction effects due to an a priori 3-dimensional conductivity model. However, the most substantial improvements entail the application of a mechanism termed Selective Infinite Variance Weighting (SIVW), which mitigates the effects of non-zero mean systematic noise and allows for the exploitation of gradient information from the low-altitude Swarm satellite pair to determine small-scale lithospheric fields, and an improvement in the treatment of attitude error due to noise in star-tracking systems over previously established methods. The advanced CI algorithm is validated by applying it to synthetic data from a full simulation of the Swarm mission, where it is found to significantly exceed all mandatory and most target accuracy requirements.

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