[GRASS-SVN] r32900 - grass/trunk/raster/r.terraflow
svn_grass at osgeo.org
svn_grass at osgeo.org
Tue Aug 19 17:25:20 EDT 2008
Author: neteler
Date: 2008-08-19 17:25:19 -0400 (Tue, 19 Aug 2008)
New Revision: 32900
Modified:
grass/trunk/raster/r.terraflow/r.terraflow.html
Log:
applied docs patch from #197
Modified: grass/trunk/raster/r.terraflow/r.terraflow.html
===================================================================
--- grass/trunk/raster/r.terraflow/r.terraflow.html 2008-08-19 18:54:48 UTC (rev 32899)
+++ grass/trunk/raster/r.terraflow/r.terraflow.html 2008-08-19 21:25:19 UTC (rev 32900)
@@ -29,7 +29,7 @@
<table width="80%" align=center>
<tr>
<th><img src="rterraflow_dir2.png" alt="[SFD]" border=0></th>
- <th><img src="rterraflow_dir3.png" alt="[SFD]" border=0></th>
+ <th><img src="rterraflow_dir3.png" alt="[MFD]" border=0></th>
</tr>
<tr>
<th>Flow direction to steepest<br> downslope neighbor (SFD).</th>
@@ -76,7 +76,7 @@
<b>d8cut</b> option, then
the flow of this cell is routed to its neighbors using the SFD (D8)
model. This option affects only the flow accumulation raster and is
-meaningfull only for MFD flow (i.e. if the -s flag is not used); If
+meaningful only for MFD flow (i.e. if the -s flag is not used); If
this option is used for SFD flow it is ignored. The default value of
<b>d8cut</b> is <i>infinity</i>.
@@ -148,7 +148,7 @@
For instance, if <em>r.terraflow.short</em> is used with floating
point raster data (FCELL or DCELL), the values of the elevation will
be truncated as shorts. This may create artificial flat areas, and the
-outpus of <em>r.terraflow.short</em> may be less realistic than those
+output of <em>r.terraflow.short</em> may be less realistic than those
of <em>r.terraflow</em> on floating point raster data.
The outputs of <em>r.terraflow.short</em> and <em>r.terraflow</em> are
@@ -199,20 +199,20 @@
<dt>Original version of program: The <a
href="http://www.cs.duke.edu/geo*/terraflow/">TerraFlow</a> project,
1999, Duke University.
- <dd><a href="http://www.cs.duke.edu/~large/">Lars Arge</a>,
+ <dd><a href="http://www.daimi.au.dk/~large/">Lars Arge</a>,
<a href="http://www.cs.duke.edu/~chase/">Jeff Chase</a>,
<a href="http://www.env.duke.edu/faculty/bios/halpin.html">Pat Halpin</a>,
- <a href="http://www.cs.duke.edu/~laura/">Laura Toma</a>,
+ <a href="http://www.bowdoin.edu/~ltoma/">Laura Toma</a>,
<a href="http://www.env.duke.edu/faculty/bios/urban.html">Dean Urban</a>,
- <a href="http://www.cs.duke.edu/~jsv/">Jeff Vitter</a>,
- <a href="http://www.cs.duke.edu/~rajiv/">Rajiv Wickremesinghe</a>.
+ <a href="http://www.science.purdue.edu/jsv/">Jeff Vitter</a>,
+ Rajiv Wickremesinghe.
<dt>Porting for GRASS, 2002:
- <dd> <a href="http://www.cs.duke.edu/~large/">Lars Arge</a>,
+ <dd> <a href="http://www.daimi.au.dk/~large/">Lars Arge</a>,
<a href="http://skagit.meas.ncsu.edu/~helena/index.html">Helena Mitasova,</a>
- <a href="http://www.cs.duke.edu/~laura/">Laura Toma</a>.
+ <a href="http://www.bowdoin.edu/~ltoma/">Laura Toma</a>.
- <dt>Contact: <a href="mailto:laura at cs.duke.edu"> Laura Toma</a></dt>
+ <dt>Contact: <a href="mailto:ltoma at bowdoin.edu "> Laura Toma</a></dt>
</dl>
@@ -239,9 +239,9 @@
Flow computation on massive grid terrains</a>.
Lars Arge, Jeffrey S. Chase, Patrick N. Halpin, Laura Toma,
Jeffrey S. Vitter, Dean Urban and Rajiv Wickremesinghe.
- To appear in <em>GeoInformatica, International Journal on
+ In <em>GeoInformatica, International Journal on
Advances of Computer Science for Geographic Information
- Systems</em>.
+ Systems</em>, 7(4):283-313, December 2003.
</ol>
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