[cig-commits] r8120 - doc/CitcomS/manual

[tan2 at geodynamics.org]

Author: tan2
Date: 2007-10-16 12:06:34 -0700 (Tue, 16 Oct 2007)
New Revision: 8120

Modified:
   doc/CitcomS/manual/citcoms.lyx
Log:
Cookbook 9, finished

Modified: doc/CitcomS/manual/citcoms.lyx
===================================================================
--- doc/CitcomS/manual/citcoms.lyx	2007-10-16 02:16:21 UTC (rev 8119)
+++ doc/CitcomS/manual/citcoms.lyx	2007-10-16 19:06:34 UTC (rev 8120)
@@ -7902,7 +7902,7 @@
  initial temperature (1), the number of nodal lines of the perturbation
  in the longitudinal direction, e.g., the spherical harmonic order (3), the
  number of nodal lines in the latitudinal direction, e.g., the spherical harmonic
- degree (2), which layer the perturbation is on (5), and the amplitude of
+ degree (2), which layer the pertubation is on (5), and the amplitude of
  the perturbation (0.05).
  Note that although the number of perturbations is assigned here as 
 \family typewriter
@@ -9872,7 +9872,7 @@
 \begin_layout Standard
 This example is a benchmark problem for compressible thermal convection.
  The Stokes solver in CitcomS has been benchmarked and validated against
- a semi-analytical solution.
+ semi-analytical solution.
  However, no analytical solution exists for the benchmark on the energy
  equation solver, which is nonlinear.
  The steady-state solution is usually used for the comparison with other
@@ -9972,7 +9972,7 @@
 \begin_layout Standard
 The initial temperature is a conductive profile with a single spherical
  harmonic perturbation.
- The perturbation is located at the mid-depth and is defined as: 
+ The pertubation is located at the mid-depth and is defined as: 
 \begin_inset Formula \[
 mag\times\sin\left(\frac{(r-r_{in})\pi}{r_{out}-r_{in}}\right)\left(\sin(m\phi)+\cos(m\phi)\right)P_{lm}(\cos\theta)\]
 
@@ -11243,12 +11243,64 @@
 \end_layout
 
 \begin_layout Standard
-(TODO) The final step.
- The isosurface is at 0.8.
- The resolution of both meshes is reduced approximately three-folds for
- better visualization.
+The results for this problem are presented in Figure 
+\begin_inset LatexCommand ref
+reference "fig:Cookbook-9"
+
+\end_inset
+
+.
+ The plume head spreads below the lithosphere, and the plume conduit is
+ elongated in the ridge-parallel direction.
+ The lithosphere subducts at the left and right edges of the csolver.
+ The domain of csolver could have been bigger so that the plume could be
+ further away from the subducted slabs.
+ 
 \end_layout
 
+\begin_layout Standard
+\begin_inset Float figure
+placement H
+wide false
+sideways false
+status open
+
+\begin_layout Standard
+\align center
+\begin_inset Graphics
+	filename /Users/tan2/cig/doc/CitcomS/manual/graphics/cookbook9.png
+
+\end_inset
+
+
+\end_layout
+
+\begin_layout Standard
+\begin_inset Caption
+
+\begin_layout Standard
+\begin_inset LatexCommand label
+name "fig:Cookbook-9"
+
+\end_inset
+
+Cookbook 9: The plume head spreads below the lithosphere, and the plume
+ conduit is elongated in the ridge-parallel direction.
+ The temperature isosurface is at 0.8.
+ The grid spacings of both meshes are reduced approximately three-folds
+ for better visualization.
+\end_layout
+
+\end_inset
+
+
+\end_layout
+
+\end_inset
+
+
+\end_layout
+
 \begin_layout Part
 Appendices
 \end_layout