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<H1><A NAME="SECTION001450000000000000000"></A>
<A NAME="10527"></A>
<BR>
6.5 A 3-D illuminated surface in black and white
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<P>
Instead of a mesh plot we may choose to show 3-D surfaces using
artificial illumination.  For this example we will use
<A NAME="tex2html388"
  HREF="../grdmath.html"><I><B>grdmath</B></I></A><A NAME="10537"></A> to make a grdfile that contains the surface given
by the function <!-- MATH
 $z(x, y) = \cos (2\pi r/8)\cdot e^{-r/10}$
 -->
<IMG
 WIDTH="183" HEIGHT="37" ALIGN="MIDDLE" BORDER="0"
 SRC="img102.gif"
 ALT="$z(x, y) = \cos (2\pi r/8)\cdot e^{-r/10}$">, where
<!-- MATH
 $r^2 = (x^2 + y^2)$
 -->
<IMG
 WIDTH="94" HEIGHT="35" ALIGN="MIDDLE" BORDER="0"
 SRC="img103.gif"
 ALT="$r^2 = (x^2 + y^2)$">.  The illumination is obtained by passing
two grdfiles to <A NAME="tex2html389"
  HREF="../grdview.html"><I><B>grdview</B></I></A><A NAME="10546"></A>: One with the <I>z</I>-values
(the surface) and another with intensity values (which should
be in the <IMG
 WIDTH="16" HEIGHT="29" ALIGN="MIDDLE" BORDER="0"
 SRC="img53.gif"
 ALT="$\pm$">1 range).  We use <A NAME="tex2html390"
  HREF="../grdgradient.html"><I><B>grdgradient</B></I></A><A NAME="10555"></A> to compute
the horizontal gradients in the direction of the artificial
light source.  The <U>gray.cpt</U> file only has one line that states
that all <I>z</I> values should have the gray level 128.  Thus,
variations in shade are entirely due to variations in gradients,
or illuminations.  We choose to illuminate from the SW and view
the surface from SE:

<P>

<P>

<BR>

<P>
<BR CLEAR="ALL">
<HR>
<BR>
<PRE>
grdmath -R-15/15/-15/15 -I0.3 X Y HYPOT DUP 2 MUL PI MUL 8 DIV COS EXCH NEG 10 DIV EXP MUL \
   = sombrero.grd
echo '-5    128    5    128' &gt;! gray.cpt
grdgradient sombrero.grd -A225 -Gintensity.grd -Nt0.75
grdview sombrero.grd -JX6i -JZ2i -B5/5/0.5SEwnZ -N-1/255/255/255 -Qs -Iintensity.grd -X1.5i -K \
   -Cgray.cpt -R-15/15/-15/15/-1/1 -E120/30 -U/-1.25i/-0.75i/"Example 5 in Cookbook" &gt;! example_05.ps
echo "4.1 5.5 50 0 33 2 z(r) = cos (2@~p@~r/8) * e@+-r/10@+" | pstext -R0/11/0/8.5 -Jx1i -O \
   &gt;&gt; example_05.ps
\rm -f gray.cpt sombrero.grd intensity.grd .gmtcommands
</PRE>

<P>
<BR>

<BR>

<P>
<BR CLEAR="ALL">
<HR>
<P>
The variations in intensity could be made more dramatic by
using <A NAME="tex2html391"
  HREF="../grdmath.html"><I><B>grdmath</B></I></A><A NAME="10617"></A> to scale the intensity file before
running <A NAME="tex2html392"
  HREF="../grdview.html"><I><B>grdview</B></I></A><A NAME="10626"></A>.  For very rough data sets one may
improve the smoothness of the intensities by passing the
output of <A NAME="tex2html393"
  HREF="../grdgradient.html"><I><B>grdgradient</B></I></A><A NAME="10635"></A> to <A NAME="tex2html394"
  HREF="../grdhisteq.html"><I><B>grdhisteq</B></I></A><A NAME="10644"></A>.  The
shell-script above will result in a plot like the one in
Figure&nbsp;<A HREF="node78.html#fig:GMT_example_05">6.5</A>.

<P></P>
<DIV ALIGN="CENTER"><A NAME="fig:GMT_example_05"></A><A NAME="10653"></A>
<TABLE>
<CAPTION ALIGN="BOTTOM"><STRONG>Figure 6.5:</STRONG>
3-D illuminated surface</CAPTION>
<TR><TD><IMG
 WIDTH="500" HEIGHT="358" BORDER="0"
 SRC="img104.gif"
 ALT="\begin{figure}\centering\epsfig{figure=eps/GMT_example_05.eps}\end{figure}"></TD></TR>
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<ADDRESS>
Paul Wessel
2001-04-18
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