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eso-midas-doc-15SEPpl1.0-2.mga6.armv5tl.rpm

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<H1><A NAME="SECTION001030000000000000000">
Geometric Correction</A>
</H1>

<P>
An accurate two dimensional geometric correction over the entire frame 
is an important part of the whole reduction process. It strongly affects 
velocity measurements along the slit and is very critical even for 
point sources if narrow night sky lines shall be properly subtracted. 
If the spectrum contains only a point source the 
user may prefer to extract it from the 2D image (<TT>EXTRACT/LONG</TT>) 
and then proceed with the normal one-dimensional spectral reduction.

<P>
On the other hand, if the spatial information along the slit is of no 
interest and night sky lines do not have to be corrected for, much time 
can be saved by properly averaging the signal along the slit (<TT>EXTRACT/AVERAGE</TT>).

<P>
The full geometrical correction of long-slit spectra is a 
transformation from the raw pixel coordinates (<I>X</I>, <I>Y</I>) to the sampling space

<!-- MATH: $(\lambda, s)$ -->
<IMG
 WIDTH="10" HEIGHT="44" ALIGN="MIDDLE" BORDER="0"
 SRC="img242.gif"
 ALT="$(\lambda, s)$">,
where <IMG
 WIDTH="42" HEIGHT="56" ALIGN="BOTTOM" BORDER="0"
 SRC="img243.gif"
 ALT="$\lambda$">
is the wavelength and 
<I>s</I> is an angular coordinate in the sky along the slit. Logically, 
it often makes sense 
to separate the geometrical transformation into two orthogonal components: the 
dispersion relation 
<!-- MATH: $\lambda = \lambda(X, Y)$ -->
<IMG
 WIDTH="78" HEIGHT="44" ALIGN="MIDDLE" BORDER="0"
 SRC="img244.gif"
 ALT="$\lambda = \lambda(X, Y)$">,
which can be obtained from 
an arc spectrum with a fully illuminated slit and the distortion along the 
slit 
<!-- MATH: $s = s(X, Y)$ -->
<I>s</I> = <I>s</I>(<I>X</I>, <I>Y</I>), which can be derived from the continuum spectra of point 
sources. Practically, these two transformations should, whenever possible, 
be combined into one before rectifying the data, because this saves one
non-linear rebinning step, each of which necessarily leading to some loss of 
information. 

<P>
As far as the reduction is concerned, the easiest way to achieve this is 
to observe the comparison lamp used for wavelength calibration through a 
a pin-hole mask. (Of course, this method can account only for instrumental 
distortions, not for differential atmospheric refraction, <I>etc.</I>) 

<P>
In the presence of strong distortions along the slit, a 2-D modeling must 
be attempted and the command <TT>RECTIFY/LONG</TT> could be considered.
If distortions along the slit can be neglected or 
suitably corrected for in a separate step, a 2-D modeling of the dispersion 
relation is still a valid approach. However, a separate reduction of detector 
row after detector row along the slit, then, often is a superior alternative. 
A broad overview of the major options is given in the next subsections; 
<B>a detailed comparison and a Cookbook for the usage of the two methods 
are provided in Appendix&nbsp;<A HREF="node497.html#long_slit_spectra">G</A>.</B> 

<P>
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<LI><A NAME="tex2html3036"
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<LI><A NAME="tex2html3037"
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<LI><A NAME="tex2html3038"
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<LI><A NAME="tex2html3039"
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<ADDRESS>
<I>Petra Nass</I>
<BR><I>1999-06-15</I>
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