Up: Spectral decomposition by genetic
Subsections
To test Ga-GA on real data we chose to analyse a spectral
region in the SUMER wavelength range that is known to suffer from
blending problems, both between spectra of different optical orders
as well as just wavelength coincidences. Those problems resulting
from blends between lines that happen to overlap in the first and
second grating orders can be decomposed experimentally, and thus
serve as a limited check on the the GA approach.
The dataset analyzed here was obtained on October 26th 1996, with
the
arcsecond slit crossing the north polar limb,
using SUMER's B detector. Data were acquired in the 1400 Å
spectral region, containing strong lines of Siiv,
Oiv, and Oiii (in second order), as well as other
weaker lines.
The observing sequence was designed to obtain data between 1399 and
1408 Å (and in the second order spectrum with wavelengths
at half of this range) on both the bare and KBr coated part of the
detector, sequentially. The exposure time on the KBr part was 180
seconds, and 360 seconds on the bare part. The bare and KBr regions of
the detector have very different sensitivities to first and second
order spectra. Assuming that the spectra did not change
significantly between the bare and KBr exposures, the different
count rates acquired on the two regions allow one to decompose the
spectrum analytically into first and second order components, I1
and I2 through the following equations
|  |
(5) |
|  |
(6) |
where
and
refer to the count rates per pixel
per second on the KBr and bare parts of the detector, I1, I2
are intensities of the first and second order spectra, and k1,
k2, b1, b2, are (known) instrument sensitivities defined
through these equations. Figure 8, top panel, shows
and its components, k1 I1 and k2 I2. Values for
I1 and I2 were obtained using measurements of
,
and instrumental sensitivities discussed by Judge
et al. (1997).
Figure 8 also shows
and its components,
in the bottom panel.
 |
Figure 8:
The 1400 Å region of the solar spectrum as measured using
the SUMER instrument (see text for details). The top panel shows
the average spectrum, in counts/pixel/second, recorded on the KBr
region of the detector. Positions of known strong lines are marked-
the positions of lines of O III are marked assuming that they are
formed in the second order. The bottom panel shows the same thing,
but recorded on the bare part of the detector. The lines plotted
with symbols show the spectral decomposition into first and second
order lines using the known sensitivities from SUMER |
In each case the count rates are averaged over
300 spatial pixels, including the solar limb, and time during the
exposures.
Shown in the top panel of Fig. 9 is a decomposition
performed using Ga-GA based only upon the
spectrum shown in the upper panel of Fig. 8. This is
simply a "blind" fit, using no prior information about
the spectrum, except that we expect between 16 and 20 Gaussians to be
present with on constant background. Such "blind" fits show that we
can obtain a reliable decomposition of the entire spectrum. An example
where a "blind" run is significantly better than one where a
priori knowledge is used to aid in the decomposition is given below
(see Table 4).
 |
Figure 9:
Comparison between Ga-GA decomposition and the analytic
decomposition of the SUMER spectrum in Fig. 8. The
top panel shows the decomposition from the Ga-GA algorithm
using only the KBr data from the top panel of
Fig. 8. The bottom panel shows the decomposition
from a single run of Ga-GA using constrained wavelengths in
the fitness calculation. See Table 4 for the details of the runs with
constrained wavelengths |
Usually, extra information about the spectrum is known, and it may
be needed for some cases. This information can be "hard-wired" into
Ga-GA easily. For example, we could demand that the spectral
decomposition must not contain spectral detail narrower than the
instrumental width (
). Or, we could specify that
relative positions (or intensities) of lines from the same ion,
known to great accuracy from laboratory measurement, be fixed to
certain values. Such constraints can be incorporated into the GA
through a simple modification of the fitness evaluation,
Eq. (3). For such an example we might use:
|  |
(7) |
| |
where we introduce the additional constants Ci and Dij to
control the "trade-off" between
and the newly incorporated
information, and where
will weight the
optimization against features narrower than
.A future version of Ga-GA may take advantage of this
additional information to act as desktop on-line plasma analysis
package. Recall however, that the number of parameters in the
calculation effects the rate of convergence (Sect. 3.1
and Sect. 3.2).
The lower panel of Fig. 9 shows the results of a
Ga-GA decomposition where we have included a line list of all
the lines marked in upper panel of Fig. 8, the
implementation of this is discussed below. The "fixed" wavelength
decomposition
(see results
in Table 4) tells us additional information about the spectrum;
there is an average redshift of 0.070 Å of the lines in the
list from their reference position. This corresponds to a velocity
of around 10 km s-1. The comparison of the contributions between
first and second order lines in the 1404- 1408 Å region
shows that Ga-GA can successfully decompose a real,
convoluted spectrum, into meaningful components.
Table 4:
This table contains the results of Ga-GA analysing
the SUMER spectrum of Fig. 8 where the wavelengths,
(Å), intensities,
, and widths
(Å) are the mean
values of a ten run ensemble.
indicates that, in this
wavelength range, a line of Arviii at
Å (in second order) dominates the emission,
as is clear from inspection of images shown by Judge
et al. (1997) but this was not
given in the line list. This line was detected in the "blind"
decomposition of Sect. 4 (
Å,
IG=0.030 and WG= 0.151 Å) with correspondingly different
measurements for the two lines of Siii. This result
illustrates that a priori information (in this case, the line
list), must be correct or erroneous results will occur. Mean
standard deviations in
and
are 0.002 and 0.001 respectively
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Up: Spectral decomposition by genetic
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