[cig-commits] r8222 - doc/CitcomS/manual

[sue at geodynamics.org]

Author: sue
Date: 2007-11-07 11:00:42 -0800 (Wed, 07 Nov 2007)
New Revision: 8222

Modified:
   doc/CitcomS/manual/citcoms.lyx
   doc/CitcomS/manual/citcoms.pdf
Log:
minor changes; new pdf

Modified: doc/CitcomS/manual/citcoms.lyx
===================================================================
--- doc/CitcomS/manual/citcoms.lyx	2007-11-07 18:07:56 UTC (rev 8221)
+++ doc/CitcomS/manual/citcoms.lyx	2007-11-07 19:00:42 UTC (rev 8222)
@@ -9761,8 +9761,7 @@
 \family typewriter
 Solver=multigrid
 \family default
-) for small problems (e.g.
- less than 17
+) for small problems (e.g., less than 17
 \begin_inset Formula $\times$
 \end_inset
 
@@ -10151,8 +10150,8 @@
 \begin_layout Standard
 We are interested in the geoid, dynamic topography, and heat flux.
  The dynamic topography and heat flux are computed on the surface grids.
- The geoid is computed in the spherical harmonics, with maximal degree of
- 
+ The geoid is computed in the spherical harmonics, with a maximal degree
+ of 
 \family typewriter
 20
 \family default
@@ -10227,8 +10226,7 @@
 \family typewriter
 Solver=cgrad
 \family default
-) for bigger problems (e.g.
- more than 17
+) for bigger problems (e.g., more than 17
 \begin_inset Formula $\times$
 \end_inset
 
@@ -10679,7 +10677,7 @@
 .
  There are 3 columns in the file, which are (longitude, latitude, geoid).
  The geoid is in a unit of meters.
- Several dimensional constants are required for the computation of geoid.
+ Several dimensional constants are required for the computation of the geoid.
  These constants have sensible default values (in SI units) for the Earth.
  Note that the temperature drop from the core-mantle boundary to the surface
  (

Modified: doc/CitcomS/manual/citcoms.pdf
===================================================================
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