[cig-commits] r14978 - doc/CitcomS/manual

sue at geodynamics.org sue at geodynamics.org
Mon May 11 11:08:07 PDT 2009


Author: sue
Date: 2009-05-11 11:08:06 -0700 (Mon, 11 May 2009)
New Revision: 14978

Modified:
   doc/CitcomS/manual/citcoms.lyx
Log:
fixed typos

Modified: doc/CitcomS/manual/citcoms.lyx
===================================================================
--- doc/CitcomS/manual/citcoms.lyx	2009-05-11 15:27:43 UTC (rev 14977)
+++ doc/CitcomS/manual/citcoms.lyx	2009-05-11 18:08:06 UTC (rev 14978)
@@ -1,4 +1,4 @@
-#LyX 1.5.1 created this file. For more info see http://www.lyx.org/
+#LyX 1.5.3 created this file. For more info see http://www.lyx.org/
 \lyxformat 276
 \begin_document
 \begin_header
@@ -12110,7 +12110,7 @@
  and install it on your machine, which requires a Fortran 90 compiler and
  a cluster, or you can go to 
 \begin_inset LatexCommand htmlurl
-name "CIG seismic portal"
+name "CIG Seismology Web Portal"
 target "crust.geodynamics.org/portals/seismo/"
 
 \end_inset
@@ -12164,14 +12164,14 @@
 \end_inset
 
 .
- In their paper, the (depth dependent) temperature and composition derivates
+ In their paper, the (depth dependent) temperature and composition derivatives
  of seismic velocities are given as polynomial coefficients.
  Note that the paper has its own reference profile, and is only valid between
  1000 km < depth < 2600 km.
  We will extend the model to whole mantle and use PREM as the reference
  profile.
- This clearly over-stretching the model, but we are using it for demonstration
- purpose.
+ This clearly is over-stretching the model, but we are using it for demonstratio
+n purposes.
 \end_layout
 
 \begin_layout LyX-Code
@@ -12432,27 +12432,27 @@
 \end_layout
 
 \begin_layout Standard
-Using your favorite browser, go to the homepage of 
+Using your favorite browser, go to the 
 \begin_inset LatexCommand htmlurl
-name "CIG seismic portal"
-target "crust.geodynamics.org/portals/seismo/"
+name "CIG Seismology Web Portal"
+target "https://crust.geodynamics.org/portals/seismo/"
 
 \end_inset
 
 .
  Free registration is required to use the portal.
  Your initial account has 10,000 SUs (CPU-hours) allocated.
- A short (20 minute of seismograms), low-resolution SPECFEM3D_GLOBE run
+ A short (20 minutes of seismograms), low-resolution SPECFEM3D_GLOBE run
  consumes about 450 SUs.
  A short, high-resolution SPECFEM3D_GLOBE run consumes about 1,000 SUs.
  Further SUs can be allocated upon request.
 \end_layout
 
 \begin_layout Standard
-After you login to the portal, take a few minutes to read the instruction
- and familiar yourself with the interface.
- You will see a toolbar with big icons on the top and several gray-out tabs
- below the toolbar.
+After you login to the portal, take a few minutes to read the instructions
+ and familiarize yourself with the interface.
+ You will see a toolbar with big icons on the top and several grayed-out
+ tabs below the toolbar.
  The toolbar allows you to specify the earthquake source (
 \family typewriter
 Events
@@ -12511,8 +12511,8 @@
  As you might have guessed from the filename, the code will generate an
  isotropic mantle without overlaid by a 3D crust, such as the CRUST2.0 model.
  The 3D crust model obeys the continent-ocean distribution of current Earth.
- Since our CitcomS model has no notation on where is Pacific and where is
- Asia, we do not want to impose a 3D crust model.
+ Since our CitcomS model has no notation on where is the Pacific and where
+ is Asia, we do not want to impose a 3D crust model.
  You can untar the file by running:
 \end_layout
 
@@ -12638,12 +12638,12 @@
  will be replaced by the absolute path when the tar file is expanded by
  the portal.
  Second, the tar file will be distributed to all computer nodes when portal
- launchs the job.
+ launches the job.
  Third, the subdirectory 
 \family typewriter
 shared/
 \family default
- is special such that files in this directory will not be distrubted to
+ is special such that files in this directory will not be distributed to
  all computer nodes.
  Data files of huge size should be put in this directory.
  You might want to edit 
@@ -12677,7 +12677,7 @@
 \family typewriter
 cookbook10.tar.gz
 \family default
- from the dialogue, then clicking on the 
+ from the resulting dialog box, then clicking on the 
 \family typewriter
 Upload
 \family default
@@ -12686,7 +12686,7 @@
 \family typewriter
 3D Models
 \family default
- icon again, you will see 
+ icon again; you will see 
 \family typewriter
 cookbook10
 \family default
@@ -12715,9 +12715,9 @@
 \family typewriter
 New
 \family default
- tab (6), and select the parameters as shown in the figure above and save
- the parameters for later use.
- We will use a global mesh that is capable of resolving seismic wave of
+ tab (6), select the parameters as shown in the figure above, and save the
+ parameters for later use.
+ We will use a global mesh that is capable of resolving seismic waves of
  27 second period.
  Since CitcomS mesh is a perfect sphere, you need to disable 
 \family typewriter
@@ -12732,7 +12732,7 @@
 \family typewriter
 oceans
 \family default
- is disabled because we don't have 3D crust.
+ is disabled because we don't have a 3D crust.
 \end_layout
 
 \begin_layout Standard
@@ -12815,7 +12815,8 @@
 stations.cookbook10
 \family default
  in the cookbook directory.
- The stations are on the Equator and is 70 to 100 degree away from the source.
+ The stations are on the Equator and are 70 to 100 degrees away from the
+ source.
  
 \family roman
 \series medium
@@ -12897,7 +12898,7 @@
 \family typewriter
 New
 \family default
- tab (8), select our recectly uploaded event, stations and parameters.
+ tab (8), and select our recently uploaded event, stations and parameters.
  Set the record length to 30 minutes, which will give us synthetic seismograms
  of 30 minutes.
  Click the 
@@ -12923,16 +12924,16 @@
 \begin_layout Standard
 You will be presented with a summary of the simulation settings, including
  a map showing the location of the events and stations.
- After you have review all settings, scroll to the bottom of the page.
+ After you have reviewed all settings, scroll to the bottom of the page.
  Click on the 
 \family typewriter
 Start
 \family default
  button.
- The request of simulation will be sent to the TeraGrid supercomputing center.
+ The request for the simulation is sent to the TeraGrid supercomputing center.
  Your simulation will be waiting in the queue and will be launched within
  several hours.
- You can log off the portal now.
+ You can log off the portal for now.
 \end_layout
 
 \begin_layout Standard
@@ -12953,8 +12954,8 @@
 \family typewriter
 Runs
 \family default
- icon, there is a list of finished and unfinished runs.
- Click on the finished run, you will see a list of output.
+ icon, where there is a list of finished and unfinished runs.
+ Click on the finished run, and you will see a list of output.
  Click on the 
 \family typewriter
 specfem3dglobe.tar.gz
@@ -12993,7 +12994,7 @@
 
 \end_inset
 
- and the dimensional parameters in 
+ and the dimensional parameters in the 
 \family typewriter
 [CitcomS.solver.const]
 \family default
@@ -13031,10 +13032,12 @@
 \begin_inset Formula $90^{\circ}$
 \end_inset
 
-range.``
+ range.
 \end_layout
 
 \begin_layout Standard
+\noindent
+\align center
 \begin_inset Float figure
 wide false
 sideways false
@@ -13061,14 +13064,9 @@
 
 \end_inset
 
-The equatorial slice of temperature from CitcomS result. Three S wave paths
- probing the mantle are shown.
+The equatorial slice of temperature from the CitcomS result.
+ Three S wave paths probing the mantle are shown.
  
-\begin_inset Note Comment
-status open
-
-\begin_layout Standard
-TODO: plotting composition, density and dVs slices.
 \end_layout
 
 \end_inset
@@ -13081,15 +13079,10 @@
 
 \end_layout
 
-\end_inset
-
-
-\end_layout
-
 \begin_layout Standard
 The synthetic seismograms need to be post-processed.
- The post-processing programs we will use can be downloaded from the potral.
- Follow the instruction on portal to build the programs.
+ The post-processing programs we will use can be downloaded from the portal.
+ Follow the instructions on the portal to build the programs.
  We will band-pass filter within the period of 30 and 500 seconds, and convolve
  the synthetics with a gaussian source time function of 50 seconds half
  duration, and append 



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