The model was derived with handpicked transverse component waveforms,
including:
1. SH body waves (S, SS, S3, S4, ScS, ScS2, ScS3, Sdiff and corresponding depth phases: sS, etc...),
down to a corner frequency of 32 sec
2. 1st & 2nd orbit Love waves
3. 1st & 2nd orbit higher modes
down to a corner frequency of 70 sec
The theoretical framework is a normal mode asymptotic formalism, including both
along branch and across branch coupling,
which provides broadband kernels
for body waveforms and surface waves (NACT).
Ray theory assumes that the sensitivity to structure of body waves is
limited to the infinitesimal ray path and uniform along the ray.
On the
other hand, standard surface wave theory ("path average" approximation)
assumes that the sensitivity kernel is 1D,
that is, depends only on
the average structure between the source and the receiver. The NACT approach takes into account
the finite width
of the sensitivity kernel of a body wave (or higher mode surface waves) around the infinitesimal ray,
and the variation
of the sensitivity along the ray.
--- red --->This framework allows the inversion of complete seismogram waveforms, with
accurate 2D sensitivity kernels.
Xiang-Dong Li and Barbara Romanowicz , "Comparison of global waveform inversions with and without considering
--- red --->
The SAW24B16 model is described in :
Charles Mégnin and Barbara Romanowicz , "The shear velocity structure of the mantle from the inversion of of body,
--- red --->
---red --->
The theory used to develop the model is described in :
cross-branch modal coupling", Geophys. J. Int. (1995) 121, 695-709. (view Abstract)
surface and higher modes waveforms", Geophys. J. Int, 143,709-728, 2000. Download a preprint.(1.2 Mb)
Alternatively, download SAW24B16 coefficients, the code to read them, (65 Mb)
and the readme file.
For all enquiries, please contact Barbara Romanowicz:
barbara@seismo.berkeley.edu Last update : 2/15/2003