[cig-commits] r12889 - in mc/2D/ConMan/trunk/doc: . images

[sue at geodynamics.org]

Author: sue
Date: 2008-09-16 11:21:56 -0700 (Tue, 16 Sep 2008)
New Revision: 12889

Modified:
   mc/2D/ConMan/trunk/doc/conman.lyx
   mc/2D/ConMan/trunk/doc/conman.pdf
   mc/2D/ConMan/trunk/doc/images/conman_cover.pdf
   mc/2D/ConMan/trunk/doc/images/conman_cover.psd
Log:
more editing to cover caption

Modified: mc/2D/ConMan/trunk/doc/conman.lyx
===================================================================
--- mc/2D/ConMan/trunk/doc/conman.lyx	2008-09-16 14:02:47 UTC (rev 12888)
+++ mc/2D/ConMan/trunk/doc/conman.lyx	2008-09-16 18:21:56 UTC (rev 12889)
@@ -230,20 +230,25 @@
 \end_layout
 
 \begin_layout Standard
-Pictured is the temperature field from a modified Cookbook 1 example [Blankenbac
-k et al, 1989], but with a higher 
-\begin_inset Formula $Ra=10^{6},$
+Pictured is a thermal convection model with fully developed downwellings
+ and upwellings.
+ The computation is performed on a 4
+\begin_inset Formula $\times$
 \end_inset
 
- and longer 4 
+1 rectangular domain with 256
 \begin_inset Formula $\times$
 \end_inset
 
- 1 aspect ratio (256 
-\begin_inset Formula $\times$
+64 uniform square elements.
+ Only part of the domain is shown.
+ This convection model uses a Rayleigh number of 
+\begin_inset Formula $10^{6}$
 \end_inset
 
- 64 elements).
+ and constant viscosity, with free slip velocity boundary conditions applied
+ on all sides and constant temperature boundary conditions on the bottom
+ and top layers.
  
 \end_layout
 

Modified: mc/2D/ConMan/trunk/doc/conman.pdf
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Modified: mc/2D/ConMan/trunk/doc/images/conman_cover.pdf
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Modified: mc/2D/ConMan/trunk/doc/images/conman_cover.psd
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