[cig-commits] r22560 - in seismo/3D/SPECFEM3D_GLOBE/trunk: DATA EXAMPLES/small_benchmark_run_to_test_more_complex_Earth EXAMPLES/small_benchmark_run_to_test_very_simple_Earth

[dkomati1 at geodynamics.org]

Author: dkomati1
Date: 2013-07-09 08:01:57 -0700 (Tue, 09 Jul 2013)
New Revision: 22560

Modified:
   seismo/3D/SPECFEM3D_GLOBE/trunk/DATA/Par_file
   seismo/3D/SPECFEM3D_GLOBE/trunk/EXAMPLES/small_benchmark_run_to_test_more_complex_Earth/Par_file_this_example
   seismo/3D/SPECFEM3D_GLOBE/trunk/EXAMPLES/small_benchmark_run_to_test_very_simple_Earth/Par_file_this_example
Log:
added more precise comments for the new parameters added to the Par_files


Modified: seismo/3D/SPECFEM3D_GLOBE/trunk/DATA/Par_file
===================================================================
--- seismo/3D/SPECFEM3D_GLOBE/trunk/DATA/Par_file	2013-07-09 02:12:34 UTC (rev 22559)
+++ seismo/3D/SPECFEM3D_GLOBE/trunk/DATA/Par_file	2013-07-09 15:01:57 UTC (rev 22560)
@@ -150,16 +150,20 @@
 
 # output only transverse isotropic kernels (alpha_v,alpha_h,beta_v,beta_h,eta,rho)
 # rather than fully anisotropic kernels when ANISOTROPIC_KL above is set to .true.
+# means to save radial anisotropic kernels, i.e., sensitivity kernels for beta_v, beta_h, etc.
 SAVE_TRANSVERSE_KL_ONLY         = .false.
 
-# output approximate hessian in crust mantle region
+# output approximate Hessian in crust mantle region.
+# means to save the preconditioning for gradients, they are cross correlations between forward and adjoint accelerations.
 APPROXIMATE_HESS_KL             = .false.
 
 # forces transverse isotropy for all mantle elements
-# (default is to use transverse isotropy only between MOHO and 220)
+# (default is to use transverse isotropy only between MOHO and 220).
+# means we allow radial anisotropy between the bottom of the crust to the bottom of the transition zone, i.e., 660~km depth.
 USE_FULL_TISO_MANTLE            = .false.
 
 # output kernel mask to zero out source region
+# to remove large values near the sources in the sensitivity kernels
 SAVE_SOURCE_MASK                = .false.
 
 # output kernels on a regular grid instead of on the GLL mesh points (a bit expensive)

Modified: seismo/3D/SPECFEM3D_GLOBE/trunk/EXAMPLES/small_benchmark_run_to_test_more_complex_Earth/Par_file_this_example
===================================================================
--- seismo/3D/SPECFEM3D_GLOBE/trunk/EXAMPLES/small_benchmark_run_to_test_more_complex_Earth/Par_file_this_example	2013-07-09 02:12:34 UTC (rev 22559)
+++ seismo/3D/SPECFEM3D_GLOBE/trunk/EXAMPLES/small_benchmark_run_to_test_more_complex_Earth/Par_file_this_example	2013-07-09 15:01:57 UTC (rev 22560)
@@ -151,16 +151,20 @@
 
 # output only transverse isotropic kernels (alpha_v,alpha_h,beta_v,beta_h,eta,rho)
 # rather than fully anisotropic kernels when ANISOTROPIC_KL above is set to .true.
+# means to save radial anisotropic kernels, i.e., sensitivity kernels for beta_v, beta_h, etc.
 SAVE_TRANSVERSE_KL_ONLY         = .false.
 
-# output approximate hessian in crust mantle region
+# output approximate Hessian in crust mantle region.
+# means to save the preconditioning for gradients, they are cross correlations between forward and adjoint accelerations.
 APPROXIMATE_HESS_KL             = .false.
 
 # forces transverse isotropy for all mantle elements
 # (default is to use transverse isotropy only between MOHO and 220)
+# means we allow radial anisotropy between the bottom of the crust to the bottom of the transition zone, i.e., 660~km depth.
 USE_FULL_TISO_MANTLE            = .false.
 
 # output kernel mask to zero out source region
+# to remove large values near the sources in the sensitivity kernels
 SAVE_SOURCE_MASK                = .false.
 
 # output kernels on a regular grid instead of on the GLL mesh points (a bit expensive)

Modified: seismo/3D/SPECFEM3D_GLOBE/trunk/EXAMPLES/small_benchmark_run_to_test_very_simple_Earth/Par_file_this_example
===================================================================
--- seismo/3D/SPECFEM3D_GLOBE/trunk/EXAMPLES/small_benchmark_run_to_test_very_simple_Earth/Par_file_this_example	2013-07-09 02:12:34 UTC (rev 22559)
+++ seismo/3D/SPECFEM3D_GLOBE/trunk/EXAMPLES/small_benchmark_run_to_test_very_simple_Earth/Par_file_this_example	2013-07-09 15:01:57 UTC (rev 22560)
@@ -151,16 +151,20 @@
 
 # output only transverse isotropic kernels (alpha_v,alpha_h,beta_v,beta_h,eta,rho)
 # rather than fully anisotropic kernels when ANISOTROPIC_KL above is set to .true.
+# means to save radial anisotropic kernels, i.e., sensitivity kernels for beta_v, beta_h, etc.
 SAVE_TRANSVERSE_KL_ONLY         = .false.
 
-# output approximate hessian in crust mantle region
+# output approximate Hessian in crust mantle region.
+# means to save the preconditioning for gradients, they are cross correlations between forward and adjoint accelerations.
 APPROXIMATE_HESS_KL             = .false.
 
 # forces transverse isotropy for all mantle elements
 # (default is to use transverse isotropy only between MOHO and 220)
+# means we allow radial anisotropy between the bottom of the crust to the bottom of the transition zone, i.e., 660~km depth.
 USE_FULL_TISO_MANTLE            = .false.
 
 # output kernel mask to zero out source region
+# to remove large values near the sources in the sensitivity kernels
 SAVE_SOURCE_MASK                = .false.
 
 # output kernels on a regular grid instead of on the GLL mesh points (a bit expensive)