============================================================================ OBSERVED COMPOSITE SPECTRA OF ALPHA TRIANGULI AUSTRALIS Assembled 12-5-95. Alp TrA photometry file: photometry actually used to construct the spectrum. Name FWHM Mag.+/-Unc. Eff Wvl Eff Wvl F-lam Source (Vega) (star) W/cm2/um (um) (um) SAAO-L 0.5648 -1.338 0.008 3.475 3.463 2.45E-14 Carter 1994 Spectral fragments and portions of these actually used in observed spectrum ("used" may include combination with other data where overlaps occur) Fragment Reference Total range Start and stop Average resolving (um) wavelengths (um) power KAO-NIR 1 2.90- 5.51 2.90- 4.87 160 KAO-5--9 2 4.94- 9.36 4.94- 8.97 190 KAO-8--13 3 8.80-13.08 ..... 250 LRS 4 7.67-22.74 7.67-12.59 30 KAO-Si:Bi 5 15.00-18.51 ..... 80 KAO-Si:P 6 21.90-27.08 ..... 180 LONG 7 1.25-35.00 11.00-35.00 -- References: 1,5,6. HIFOGS data of April 10 & 12, 1993 KAO flights [alp TrA/alp1 Cen] and [alp TrA/alp CMa]. 2,3. HIFOGS data of April 7, 1993 KAO flight [alp TrA/alp1 Cen] and [alp TrA/alp CMa]. The 5--9 um spectral ratio is additionally confirmed by HIFOGS data of July 22, 1994 KAO flight from Australia. 4. LRS raw data extracted from "LRSVAX" Groningen archive at NASA-Ames 7. Engelke Fn. used for T=4140K and ang. diam. of 12.40 mas (Harper 1992); we rescaled this to 9.55 mas. This Engelke Function was locked to the photometrically scaled LRS spectrum by splicing and used to replace the observations from 11.00 um. An error of 2.6% in EFn. due to effective temperature uncertainty was input for this fragment. INFORMATION ON SPLICES AND BIASES INCURRED Process Factor determined +/-Bias (%) KAO-NIR cf. photometry 1.004 0.74 KAO-5--9 splice to NIR 1.050 0.14 LRS blue/red bias -- 0.06 LRS splice to KAO 1.009 0.40 Engelke Fn. splice to LRS 0.593 0.78 ============================================================================ Notes: 1. Composite spectra are NOT tabulated at equal intervals of the wavelength, but rather at the wavelengths of the original model. 2. In most cases "total uncertainty" is the error term most appropriate to use. It is the standard deviation of the spectral irradiance and includes the local and global biases. Local and global biases are given as a percent of the irradiance. The global bias does not contribute error to flux ratios or color measurements, and may, in those cases, be removed (in the RSS sense) from the total error. ============================================================================