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author | Joseph Hunkeler <jhunkeler@gmail.com> | 2015-07-08 20:46:52 -0400 |
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committer | Joseph Hunkeler <jhunkeler@gmail.com> | 2015-07-08 20:46:52 -0400 |
commit | fa080de7afc95aa1c19a6e6fc0e0708ced2eadc4 (patch) | |
tree | bdda434976bc09c864f2e4fa6f16ba1952b1e555 /noao/twodspec/apextract/doc/approfiles.hlp | |
download | iraf-linux-fa080de7afc95aa1c19a6e6fc0e0708ced2eadc4.tar.gz |
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diff --git a/noao/twodspec/apextract/doc/approfiles.hlp b/noao/twodspec/apextract/doc/approfiles.hlp new file mode 100644 index 00000000..43ae774a --- /dev/null +++ b/noao/twodspec/apextract/doc/approfiles.hlp @@ -0,0 +1,131 @@ +.help approfiles Feb93 noao.twodspec.apextract + +.ce +Spectrum Profile Determinations + + +The foundation of variance weighted or optimal extraction, cosmic ray +detection and removal, two dimensional flat field normalization, and +spectrum fitting and modeling is the accurate determination of the +spectrum profile across the dispersion as a function of wavelength. +The previous version of the APEXTRACT package accomplished this by +averaging a specified number of profiles in the vicinity of each +wavelength after correcting for shifts in the center of the profile. +This technique was sensitive to perturbations from cosmic rays +and the exact choice of averaging parameters. The current version of +the package uses two different algorithm which are much more stable. + +The basic idea is to normalize each profile along the dispersion to +unit flux and then fit a low order function to sets of unsaturated +points at nearly the same point in the profile parallel to the +dispersion. The important point here is that points at the same +distance from the profile center should have the nearly the same values +once the continuum shape and spectral features have been divided out. +Any variations are due to slow changes in the shape of the profile with +wavelength, differences in the exact point on the profile, pixel +binning or sampling, and noise. Except for the noise, the variations +should be slow and a low order function smoothing over many points will +minimize the noise and be relatively insensitive to bad pixels such as +cosmic rays. Effects from bad pixels may be further eliminated by +chi-squared iteration and clipping. Since there will be many points +per degree of freedom in the fitting function the clipping may even be +quite aggressive without significantly affecting the profile +estimates. Effects from saturated pixels are minimized by excluding +from the profile determination any profiles containing one or more +saturated pixels as defined by the \fIsaturation\fR parameter. + +The normalization is, in fact, the one dimensional spectrum. Initially +this is the simple sum across the aperture which is then updated by the +variance weighted sum with deviant pixels possibly removed. This updated +one dimensional spectrum is what is meant by the profile normalization +factor in the discussion below. The two dimensional spectrum model or +estimate is the product of the normalization factor and the profile. This +model is used for estimating the pixel intensities and, thence, the +variances. + +There are two important requirements that must be met by the profile fitting +algorithm. First it is essential that the image data not be +interpolated. Any interpolation introduces correlated errors and +broadens cosmic rays to an extent that they may be confused with the +spectrum profile, particularly when the profile is narrow. This was +one of the problems limiting the shift and average method used +previously. The second requirement is that data fit by the smoothing +function vary slowly with wavelength. This is what precludes, for +instance, fitting profile functions across the dispersion since narrow, +marginally sampled profiles require a high order function using only a +very few points. One exception to this, which is sometimes useful but +of less generality, is methods which assume a model for the profile +shape such as a gaussian. In the methods used here there is no +assumption made about the underlying profile other than it vary +smoothly with wavelength. + +These requirements lead to two fitting algorithms which the user +selects with the \fIpfit\fR parameter. The primary method, "fit1d", +fits low order, one dimensional functions to the lines or columns +most nearly parallel to the dispersion. While this is intended for +spectra which are well aligned with the image axes, even fairly large +excursions or tilts can be adequately fit in this +way. When the spectra become strongly tilted then single lines or +columns may cross the actual profile relatively quickly causing the +requirement of a slow variation to be violated. One thought is to use +interpolation to fit points always at the same distance from the +profile. This is ruled out by the problems introduced by +image interpolation. However, there is a clever method which, in +effect, fits low order polynomials parallel to the direction defined by +tracing the spectrum but which does not interpolate the image data. +Instead it weights and couples polynomial coefficients. This +method was developed by Tom Marsh and is described in detail in the +paper, "The Extraction of Highly Distorted Spectra", PASP 101, 1032, +Nov. 1989. Here we refer to this method as the Marsh or "fit2d" +algorithm and do not attempt to explain it further. + +The choice of when to use the one dimensional or the two dimensional +fitting is left to the user. The "fit1d" algorithm is preferable since it +is faster, easier to understand, and has proved to be very robust. The +"fit2d" algorithm usually works just as well but is slower and has been +seen to fail on some data. The user may simply try both to achieve the +best results. + +What follows are some implementation details of the preceding ideas in the +APEXTRACT package. For column/line fitting, the fitting function is a +cubic spline. A base number of spline pieces is set by rounding up the +maximum trace excursion; an excursion of 1.2 pixels would use a spline of 2 +pieces. To this base number is added the number of coefficients in the +trace function in excess of two; i.e. the number of terms in excess of a +linear function. This is done because if the trace wiggles a large amount +then a higher order function will be needed to fit a line or column as the +profile shifts under it. Finally the number of pieces is doubled +because experience shows that for low tilts it doesn't matter but for +large tilts this improves the results dramatically. + +For the Marsh algorithm there are two parameters to be set, the +polynomial order parallel to the dispersion and the spacing between +parallel, coupled polynomials. The algorithm requires that the spacing +be less than a pixel to provide sufficient sampling. The spacing is +arbitrarily set at 0.95 pixels. Because the method always fits +polynomials to points at the same position of the profile the order +should be 1 except for variations in the profile shape with +wavelength. To allow for this the profile order is set at 10; i.e. a +9th order function. A final parameter in the algorithm is the number +of polynomials across the profile but this is obviously determined +from the polynomial spacing and the width of the aperture including an +extra pixel on either side. + +Both fitting algorithms weight the pixels by their variance as computed +from the background and background variance if background subtraction +is specified, the spectrum estimate from the profile and the spectrum +normalization, and the detector noise parameters. A poisson +plus constant gaussian readout noise model is used. The noise model is +described further in \fBapvariance\fR. + +As mentioned earlier, the profile fitting can be iterated to remove +deviant pixels. This is done by rejecting pixels greater than a +specified number of sigmas above or below the expected value based +on the profile, the normalization factor, the background, the +detector noise parameters, and the overall chi square of the residuals. +Rejected points are removed from the profile normalization and +from the fits. +.ih +SEE ALSO +apbackground apvariance apall apsum apfit apflatten +.endhelp |