A multiscale method is introduced using spherical (vector) wavelets for the
computation of the earth's magnetic field within source regions of ionosph
eric and magnetospheric currents. The considerations are essentially based
on two geomathematical keystones, namely (i) the Mie representation of sole
noidal vector fields in terms of toroidal and poloidal parts and (ii) the H
elmholtz decomposition of spherical (tangential) vector fields. Vector wave
lets are shown to provide adequate tools for multiscale geomagnetic modelli
ng in form of a multiresolution analysis, thereby completely circumventing
the numerical obstacles caused by vector spherical harmonics. The applicabi
lity and efficiency of the multiresolution technique is tested with real sa
tellite data. (C) 2001 Elsevier Science Ltd. All rights reserved.