Non-linear altimetric geoid inversion for lithospheric elastic thickness and crustal density

Details Non-linear altimetric geoid inversion for lithospheric elastic thickness and crustal density Non-linear altimetric geoid inversion for lithospheric elastic thickness and crustal density

Sep 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999geoji.138..667r&link_type=abstract

Geophysical Journal International, Volume 138, Issue 3, pp. 667-678.

Astronomy and Astrophysics

Astronomy

6

Geoid Anomalies, Inverse Problem, Lithospheric Flexure

Scientific paper

The inversion of high-resolution geoid anomaly maps derived from satellite altimetry should allow one to retrieve the lithospheric elastic thickness, T_e , and crustal density, rho_c . Indeed, the bending of a lithospheric plate under the load of a seamount depends on both parameters, and the associated geoid anomaly is correspondingly dependent on the two parameters. The difference between the observed and modelled geoid signatures is estimated by a cost function, J, of the two variables, T_e and rho_c . We show that this cost function forms a valley structure along which many local minima appear, the global minimum of J corresponding to the true values of the lithospheric parameters. Classical gradient methods fail to find this global minimum because they converge to the first local minimum of J encountered, so that the final parameter estimate strongly depends on the starting pair of values (T_e , rho_c ). We here implement a non-linear optimization algorithm to recover these two parameters from altimetry data. We demonstrate from the inversion of synthetic data that this approach ensures robust estimates of T_e and rho_c by activating two search phases alternately: a gradient phase to find a local minimum of J, and a tunnelling phase through high values of the cost function. The accuracy of the solution can be improved by a search in an iteratively restricted parameter subspace. Applying our non-linear inversion to the Great Meteor Seamount geoid data, we further show that the inverse problem is intrinsically ill-posed. As a consequence, minute geoid (or gravity) data errors can induce large changes in any recovery of lithospheric elastic thickness and crustal density.

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