Imaging Earth's crustal magnetic field with satellite data: a regularized spherical triangle tessellation approach
Article first published online: 25 AUG 2009
DOI: 10.1111/j.1365-246X.2009.04345.x
© 2009 The Authors Journal compilation © 2009 RAS
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How to Cite
Stockmann, R., Finlay, C. C. and Jackson, A. (2009), Imaging Earth's crustal magnetic field with satellite data: a regularized spherical triangle tessellation approach. Geophysical Journal International, 179: 929–944. doi: 10.1111/j.1365-246X.2009.04345.x
Publication History
- Issue published online: 9 OCT 2009
- Article first published online: 25 AUG 2009
- Accepted 2009 July 24. Received 2009 June 23; in original form 2009 March 20
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Keywords:
- Image processing;
- Inverse theory;
- Satellite magnetics
SUMMARY
We present a method for imaging the global crustal magnetic field at Earth's surface using a local basis representation and a minimum norm model regularization approach. The local basis consists of a spherical triangle tessellation (STT) parametrization of the radial component of the crustal field at Earth's reference spherical surface. The Green's function for Laplace's equation in spherical geometry with Neumann boundary conditions provides the necessary forward modelling scheme. We solve the inverse problem of estimating the crustal field from satellite magnetic observations by minimizing an objective function comprising a mean absolute deviation (L1-norm) measure of misfit plus a norm measuring model complexity. Both quadratic and entropy measures of field complexity are investigated. We report results from synthetic tests performed on a geophysically motivated scenario; these include a successful benchmark of the method and a comparison between quadratic and entropy regularization strategies. Applying our technique to real observations collected by the CHAMP, Ørsted and SAC-C satellites, we obtain stable images of the crustal magnetic field at Earth's surface that include sharp features with high amplitudes. We present details of two prototype crustal field models STT-CRUST-Q and STT-CRUST-E regularized using quadratic and entropy norms respectively; these provide a perspective complementary to that given by conventional spherical harmonic crustal field models.

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