[cig-commits] r21216 - seismo/3D/SPECFEM3D_GLOBE/trunk/src/specfem3D
dkomati1 at geodynamics.org
dkomati1 at geodynamics.org
Tue Jan 8 06:58:45 PST 2013
Author: dkomati1
Date: 2013-01-08 06:58:45 -0800 (Tue, 08 Jan 2013)
New Revision: 21216
Modified:
seismo/3D/SPECFEM3D_GLOBE/trunk/src/specfem3D/prepare_timerun.f90
Log:
added a comment about the factor of 2 in the scaling used to shift "mu" to the right frequency in the Earth model used
Modified: seismo/3D/SPECFEM3D_GLOBE/trunk/src/specfem3D/prepare_timerun.f90
===================================================================
--- seismo/3D/SPECFEM3D_GLOBE/trunk/src/specfem3D/prepare_timerun.f90 2013-01-07 15:44:21 UTC (rev 21215)
+++ seismo/3D/SPECFEM3D_GLOBE/trunk/src/specfem3D/prepare_timerun.f90 2013-01-08 14:58:45 UTC (rev 21216)
@@ -626,7 +626,11 @@
! anelasticity: implications for seismology and mantle composition,
! Geophys. J. R. Astron. Soc., vol. 47, pp. 41-58 (1976)
! and in Aki, K. and Richards, P. G., Quantitative seismology, theory and methods,
- ! W. H. Freeman, (1980), second edition, sections 5.5 and 5.5.2, eq. (5.81) p. 170
+ ! W. H. Freeman, (1980), second edition, sections 5.5 and 5.5.2, eq. (5.81) p. 170.
+ ! Beware that in the book of Aki and Richards eq. (5.81) is given for velocities
+ ! while we need an equation for "mu" and thus we have an additional factor of 2
+ ! in the scaling factor below and in equation (49) of Komatitsch and Tromp, Geophys. J. Int. (2002) 149, 390-412,
+ ! because "mu" is related to the square of velocity.
! rescale in crust and mantle
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