Application of regionalized multiplet stripping to the retrieval of even degree aspherical structure constraints.

This page contains supplementary material to a paper published in the Geophysical Journal International:
Application of regionalized multiplet stripping to the retrieval of even degree aspherical structure constraints
by R. Widmer-Schnidrig, Geophys. J. Int. Vol. 148, p. 201-213, 2002.

+ Download manuscript ( pdf )
+ Machine readable table of multiplet degenerate frequencies of spheroidal modes
+ Machine readable table of multiplet degenerate frequencies of fundamental toroidal modes
+ Machine readable table of aspherical structure coefficients of spheroidal modes
+ Machine readable table of aspherical structure coefficients of fundamental toroidal modes

Note: The aspherical structure coefficients, Cst, listed in the above tables are normalized as in Edmonds, A.R., Angular Momentum in Quantum Mechanics, (1960), Princeton University Press, Princeton N.J.

Intermediate results from regionalized multiplet stripping

spheroidal mode branch peak shift patterns for individual multiplets summary plots
0 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60 c2t c4t
1 11 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 c2t c4t
2 10 11 12 13 14 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 c2t c4t
3 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 41 42 43 44 45 46 47 48 49 50 c2t c4t
4 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 c2t c4t
5 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 c2t c4t
6 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 c2t c4t
7 12 17 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 c2t c4t
8 10 11 21 22 c2t c4t
9 10 11 12 13 14 15 16 18 c2t c4t
10 10 11 12 13 15 16 17 18 19 20 21 22 26 27 28 29 c2t c4t
11 10 20 21 22 23 24 28 29 30 31 32 33 34 c2t c4t
12 11 12 13 14 15 16 c2t c4t
13 16 17 18 19 20 21 22 c2t c4t
15 11 12 15 16 c2t c4t
16 18 19 20 21 c2t c4t
17 22 23 24 25 c2t c4t
19 13 14 15 c2t c4t
20 19 c2t c4t

For comments or questions send e-mail to: widmer@geophys.uni-stuttgart.de