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eso-midas-doc-13SEPpl1.2-3.mga5.i586.rpm

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<H2><A NAME="SECTION001161000000000000000">
General Description</A>
</H2>

<P>
A preliminary step to the wavelength calibration consists of extracting
the orders of the <TT>WLC</TT> image which can then be used to determine
the dispersion relation in two steps:

<P>
<UL>
<LI>The calibration lines are detected on the extracted orders by 
      means of a simple thresholding algorithm. The center of the line 
      is estimated by its center of gravity (<TT>GRAVITY</TT> method) or
      by a gaussian fit to the line profile (<TT>GAUSSIAN</TT> method). 
      This is done with the command <TT>SEARCH/ECHELLE</TT>.

<P>
<LI>A few lines are identified interactively on the 2D&nbsp;image display
      and a set of global dispersion coefficients are derived by comparing the
      identified lines with the line catalogue available in the system.
      This global model for the dispersion is a function of the wavelength
      and the spectral order number.
      Finally, dispersion coefficients for each order are computed
      using the global coefficients as a first approximation.
      A&nbsp;polynomial of degree&nbsp;2 or&nbsp;3 is sufficient to obtain, for each order, 
      a good approximation of the wavelength scale.

<P>
The command <TT>IDENTIFY/ECHELLE</TT> involves the echelle
      relation and requires the identification of two
      lines in overlapped regions of adjacent orders (method <TT>PAIR</TT>).
      The calibration can as well be performed for spectra which orders are 
      not overlapped, this time requiring a minimum of four identifications 
      (method <TT>ANGLE</TT>). Both methods are based on the echelle relation
      and therefore are not applicable if the disperser is not an echelle
      grating, as it is the case for <TT>EFOSC</TT> which involves a grism
      disperser. The method <TT>TWO-D</TT> allows to start directly the calibration
      with a two-dimensional fitting polynomial and requires more initial
      identifications. In case of several observations with the same, 
      or near the same instrumental configuration, it is possible to 
      use the global dispersion model from a previous calibration.
      The method <TT>GUESS</TT> implements this mode of operation. Two 
      additional methods <TT>RESTART</TT> and <TT>ORDER</TT> are available.
      The selection of the method is performed by assigning a value to 
      the echelle keyword <TT>WLCMTD</TT>. 

<P>
Solutions are computed either for each independent order 
      (<TT>WLCOPT=1D</TT>) or using a global bivariate polynomial 
      (<TT>WLCOPT=2D</TT>). 

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<ADDRESS>
<I>Petra Nass</I>
<BR><I>1999-06-15</I>
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