The spectrometer data consist of three types of data: (i) uncorrected spectra with header information, (ii) calibration tables, and (iii) administrative files. The spectra were extracted out of the data stream whenever an hours-confirmed source with a signal-to-noise ratio greater than 25 or a source specified as "known source" (Section V.D.4), crossed the spectrometer aperture. Extractions were also made for designated calibration sources. The spectra were linked to survey sources using index association records produced by the hours-and weeks- confirmation processors (Section V.D.7).
There were three types of calibration tables: (a) the responses of the five detectors to the internal reference source flashes and the intensities of the flashes as derived by the survey calibration processor; (b) correction tables for the relative responsivity as a function of position across the five detectors; (c) correction tables for the relative responsivity as a function of wavelength. The cross-scan and wavelength dependent responsivity tables were derived from special observations (see Section IX.B).
Processing of the data always started with the raw data. This allowed the correction procedures to be improved continuously up to the time of production of the catalog. The major processing steps are discussed below.
Single sample spikes with an amplitude greater than 8% caused by multiplexer errors (Section IX.B) were removed and replaced by an interpolated value using a simple algorithm operating on the raw data. Multiple-sample spikes were not removed but their presence was noted so that the spectrum-half would be rejected later (see Section IX.C.3).
A lookup table of 256 entries was used to convert the raw data to voltages on a linear scale. A standard reconstruction of the input-voltage to the high-pass filter from the measured output voltage was carried out. An offset correction was reset to zero whenever the sample voltage dropped below a specified threshold because of the effects of the zero clamping (Section IX.A.4).
For ease of processing, an interpolation was carried out to a standard regular grid of angular positions in the dispersion direction. Because the dispersion of the spectrograph changed rapidly as a function of the angular position (Fig. IX.A.1), the wavelength values corresponding to the standard sample values were not equidistant. Before the interpolation, allowance was made for variations in the scan speed of the telescope. For the spectra of the brighter sources (signal-to-noise ratio greater than 10) the well-defined in-scan detector edges were in-scan to center the spectrum. The centering correction reduced in-scan errors to approximately 2", corresponding to approximately 0.03 µm in wavelength.
The interpolated samples were multiplied by a responsivity
table sampled at the same standard grid. There was a table for
each of the five detectors derived from observations of
Tau (Fig. IX.B.2).
Although the software allowed selecting a different
table for each of 16 regularly spaced cross-scan positions on
the detector, the evidence for a cross-scan variation of the wavelength-dependent
gain was too weak to justify using this option.
Depending on the nominal cross-scan position of the source, a correction (Fig. IX.B.1) was applied for the decrease of responsivity towards the edges of the detectors. This correction was the weakest link in the calibration process because of the relatively large uncertainty in the cross-scan position. The correction applied is uncertain by up to 20%, although this uncertainty was decreased by the process of joining the two spectrum-halves together (see Section IX.C.2.g).
The overall responsivity depended on the individual detector, on the time and/or on the sky position. To account for these variations a correction was derived from the voltage responses to the two internal reference source flashes bracketing the time of observation. After applying the responsivity correction to a large sample of spectra the integrated fluxes in the spectra were compared to the fluxes measured by the survey array. Systematic factors of 0.75 and 1.00 were applied to the integrated spectrometer fluxes to bring them in line with the survey observations.
The two spectrum-halves (8-13 µm and 11-22 µm) were treated independently until this point. Because of uncertainties in the cross-scan position of the scan path over the detectors and therefore in the nominal cross-scan responsivity correction, the two spectrum-halves often differed by up to 15 or 20% after subtraction of a linear baseline. The overlapping portion of the spectrum-halves was used to determine another correction factor. In doing so, the nominal relative cross-scan positions were used to determine which half of the spectrum to change by the largest amount. If either half had been observed by the central part of a detector, it was considered reliably calibrated, and that portion was not changed by the joining process, and the half of the spectrum observed near the edge of a detector was shifted up or down towards the other half. If both halves were considered equally reliable, then each was scaled by the square root of the ratio between the overlapping sections. This joining process reduced the overall error in the responsivity correction to less than 10%.
Before spectra were averaged, a number of quality checks were performed on the individual measurements of the two halves of a source's spectrum. First, all measurements made within 18" of the edge of any detector were flagged. Measurements were rejected:
At least 80% of the spectra in the catalog had correlation coefficients above 70 and 60% in the short and long wavelength halves, respectively. Some 40% correlated internally with coefficients better than 80% in both spectrum-halves (see Section IX.C.4).
The spectrum-halves passing through all of the above tests were averaged using the inverse of the square of the noise as a weighting factor. At least two measurements in each of the two spectrum-halves (8-13 and 11-22 µm) had to be accepted before the spectrum could be averaged and included in the spectral catalog.
After averaging the two spectrum-halves were rejoined, giving both halves equal weight (see Section IX.C.1). Generally the join factors differed from 1.00 by only a few percent.
The averaged spectrum was convolved with the 12 µm survey
passband. The integrated flux thus obtained, was compared to the
average 12 µm survey flux of the source. The ratio between the
two fluxes is given in the low resolution spectrometer catalog
record and has a 1 dispersion around
unity of about 15%. Exceptions to this rule will be spectra with sharp
lines (classes 8 and 9; see Section IX.D.2) or
small 12 µm fluxes.
Three selection criteria were applied for inclusion in the Catalog of Low Resolution Spectra.
Four samples of sources were selected for inclusion in the catalog.
Samples a b, and c contain continuum sources and approximately 75% of the line sources of the catalog; sample d contains the remainder of the line sources.