[cig-commits] r15975 - doc/geodynamics.org/benchmarks/trunk/magma

[luis at geodynamics.org]

Author: luis
Date: 2009-11-16 14:48:56 -0800 (Mon, 16 Nov 2009)
New Revision: 15975

Modified:
   doc/geodynamics.org/benchmarks/trunk/magma/milestone1.html
   doc/geodynamics.org/benchmarks/trunk/magma/milestone2.html
   doc/geodynamics.org/benchmarks/trunk/magma/milestone3.html
Log:
Regenerated magma/milestone{1,2,3}.html files

Modified: doc/geodynamics.org/benchmarks/trunk/magma/milestone1.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/magma/milestone1.html	2009-11-16 22:44:59 UTC (rev 15974)
+++ doc/geodynamics.org/benchmarks/trunk/magma/milestone1.html	2009-11-16 22:48:56 UTC (rev 15975)
@@ -57,26 +57,27 @@
 global errors as a function of resolution are given below.</p>
 <!-- fig:2d-ridge-model -->
 <div align="center" class="figure">
-<img alt="2D Ridge Model" src="/cig/workinggroups/magma/workarea/benchmark/ridge2d126x60" />
+<img alt="2D Ridge Model" src="/cig/workinggroups/magma/workarea/benchmark/ridge2d126x60" style="width: 600px;" />
 <p class="caption">Velocity, pressure, and pressure gradients solutions and L2 errors
 for a 2D ridge model with 120x60 elements.</p>
 </div>
 <!-- fig:3d-ridge-model -->
 <div align="center" class="figure">
-<img alt="3D Ridge Model" src="/cig/workinggroups/magma/workarea/benchmark/ridge3d64x32x64" />
+<img alt="3D Ridge Model" src="/cig/workinggroups/magma/workarea/benchmark/ridge3d64x32x64" style="width: 600px;" />
 <p class="caption">Velocity, pressure, and pressure gradients solutions and L2 error
 fields for 3D ridge model.</p>
 </div>
 <!-- fig:global-pressure-gradient-errors-for-2d-ridge-model -->
 <div align="center" class="figure">
-<img alt="Global L2 Errors" src="/cig/workinggroups/magma/workarea/benchmark/ridge2dpressuregradienterrors" />
+<img alt="Global L2 Errors" src="/cig/workinggroups/magma/workarea/benchmark/ridge2dpressuregradienterrors" style="width: 600px;" />
 <p class="caption">Normalized global L2 errors.</p>
 </div>
 <!-- fig:global-pressure-gradients-for-3d-ridge-model -->
 <div align="center" class="figure">
-<img alt="Global L2 Errors - 3D Ridge Model" src="/cig/workinggroups/magma/workarea/benchmark/ridge2dpressuregradienterrors" />
+<img alt="Global L2 Errors - 3D Ridge Model" src="/cig/workinggroups/magma/workarea/benchmark/ridge2dpressuregradienterrors" style="width: 600px;" />
 <p class="caption">Normalized global L2 pressure gradient errors at varying resolutions.</p>
 </div>
+<!-- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -->
 <!-- Related Item(s) -->
 <!-- 2D Ridge Model -->
 <!-- 3D Ridge Model -->

Modified: doc/geodynamics.org/benchmarks/trunk/magma/milestone2.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/magma/milestone2.html	2009-11-16 22:44:59 UTC (rev 15974)
+++ doc/geodynamics.org/benchmarks/trunk/magma/milestone2.html	2009-11-16 22:48:56 UTC (rev 15975)
@@ -77,15 +77,51 @@
 of the smoother gradients involved), both interpolation methods converged
 at a rate much better than linear, with the cubic interpolation method
 proving far superior to the quadratic method.</p>
-<p>Related Item(s)</p>
-<blockquote>
-Gaussian Porosity Field Advection
-Ridge Model With Gaussian Porosity Field
-Semi Lagrangian Advection Scheme Test - Step Function
-Semi Lagrangian Advection Scheme Test - Gaussian Distribution
-Error Convergence for Advection Scheme - Step Function IC
-Error Convergence for Advection Scheme - Gaussian IC</blockquote>
+<!-- fig:gaussian-porosity-field-advection -->
+<div align="center" class="figure">
+<img alt="Gaussian Porosity Field Advection" src="/cig/workinggroups/magma/workarea/benchmark/milestone2gaussianporosityfield" />
+<p class="caption">Advection of Gaussian porosity field as a Stokes equation force term.
+The lower density porosity region rises due to gravity.</p>
 </div>
+<!-- fig:ridge-model-with-gaussian-porosity-field -->
+<div align="center" class="figure">
+<img alt="Ridge Model with Gaussian Porosity Field" src="/cig/workinggroups/magma/workarea/benchmark/milestone2ridgemodelgaussianporosity" />
+<p class="caption">Stokes flow with 2D ridge model boundary conditions and Gaussian porosity
+initial distribution, driven by a porosity dependent force term.</p>
 </div>
+<!-- fig:semi-lagrangian-advection-scheme-test- -step-function -->
+<div align="center" class="figure">
+<img alt="Semi-Lagrangian Advection Scheme Test - Step Function" src="/cig/workinggroups/magma/workarea/benchmark/milestone2advectionschemeteststepfunc" />
+<p class="caption">Diagonal step function initial distribution subjected to a shearing
+velocity field.</p>
+</div>
+<!-- fig:semi-lagrangian-advection-scheme-test- -gaussian-distribution -->
+<div align="center" class="figure">
+<img alt="Semi-Lagrangian Advection Scheme Test - Gaussian Distribution" src="/cig/workinggroups/magma/workarea/benchmark/milestone2advectionschemetestgaussiandist" />
+<p class="caption">Gaussian initial distribution subjected to a shearing velocity field.</p>
+</div>
+<!-- fig:error-convergence-for-advection-scheme- -step-function-ic -->
+<div align="center" class="figure">
+<img alt="Error Convergence for Advection Scheme - Step Function IC" src="/cig/workinggroups/magma/workarea/benchmark/milestone2advectionschemeconvergencestepfunc" />
+<p class="caption">Normalized global L2 errors for semi-Lagrangian advection scheme with
+a diagonal step function initial condition as a function of resolution.</p>
+</div>
+<!-- fig:error-convergence-for-advection-scheme- -gaussian-ic -->
+<div align="center" class="figure">
+<img alt="Error Convergence for Advection Scheme - Gaussian IC" src="/cig/workinggroups/magma/workarea/benchmark/ridge2dpressuregradienterrors" />
+<p class="caption">Normalized global L2 errors for semi-Lagrangian advection scheme with
+Gaussian initial distribution as a function of resolution.</p>
+</div>
+<!-- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -->
+<!-- Related Item(s) -->
+<!-- Gaussian Porosity Field Advection -->
+<!-- Ridge Model With Gaussian Porosity Field -->
+<!-- Semi Lagrangian Advection Scheme Test - Step Function -->
+<!-- Semi Lagrangian Advection Scheme Test - Gaussian Distribution -->
+<!-- Error Convergence for Advection Scheme - Step Function IC -->
+<!-- Error Convergence for Advection Scheme - Gaussian IC -->
+<!--  -->
+</div>
+</div>
 </body>
 </html>

Modified: doc/geodynamics.org/benchmarks/trunk/magma/milestone3.html
===================================================================
--- doc/geodynamics.org/benchmarks/trunk/magma/milestone3.html	2009-11-16 22:44:59 UTC (rev 15974)
+++ doc/geodynamics.org/benchmarks/trunk/magma/milestone3.html	2009-11-16 22:48:56 UTC (rev 15975)
@@ -35,10 +35,25 @@
 velocity fields have already been accurately determined. As such no tests
 were applied to validate its accuracy, however qualitatively their
 behavior is observed to be correct.</p>
-<p>Related Item(s)</p>
-<blockquote>
-Melt Model - Gaussian Porosity Driven Flow
-Melt Model - 2D Ridge with Constant Porosity</blockquote>
+<!-- fig:melt-model- -gaussian-porosity-driven-flow -->
+<div align="center" class="figure">
+<img alt="Melt Model - Gaussian Porosity Driven Flow" src="/cig/workinggroups/magma/workarea/benchmark/milestone3gaussianporositydrivenflow" />
+<p class="caption">Solid and melt velocity, pressure and pressure-gradient fields
+for Stokes flow driven by a Gaussian initial porosity dstribution.</p>
 </div>
+<!-- fig:melt-model- -2d-ridge-with-constant-porosity -->
+<div align="center" class="figure">
+<img alt="Melt Model - 2D Ridge with Constant Porosity" src="/cig/workinggroups/magma/workarea/benchmark/milestone3ridgemodelconstantphi" />
+<p class="caption">Solid and melt velocity, pressure and pressure-gradient fields
+for 2D ridge model with constant porosity. Melt velocity magnitudes
+are significantly larger near the point of discontinuity due
+to their proportionality to the pressure gradients, which
+are largest at these points.</p>
+</div>
+<!-- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -->
+<!-- Related Item(s) -->
+<!-- Melt Model - Gaussian Porosity Driven Flow -->
+<!-- Melt Model - 2D Ridge with Constant Porosity -->
+</div>
 </body>
 </html>