OBSERVED COMPOSITE SPECTRUM OF ALPHA BOO Assembled on 4-28-93 Alpha Boo photometry file: photometry actually used to construct the spectrum. Name FWHM Mag.+/-Unc. Eff Wvl Eff Wvl F-lam (Vega) (star) W/cm2/um (um) (um) (um) Kn 0.0488 -3.07 0.01 2.208 2.205 6.66E-13 Ln 0.1443 -3.15 0.01 3.782 3.762 9.39E-14 M 0.6677 -2.97 0.02 4.758 4.736 3.25E-14 8.7 1.1576 -3.12 0.01 8.753 8.730 3.46E-15 11.7 1.2008 -3.19 0.03 11.650 11.621 1.19E-15 Spectral fragments and portions of these actually used in observed spectrum Fragment Reference Total range Start and stop Average resolving (um) wavelengths (um) power NIR 1 1.22- 5.70 1.22- 4.22 50 KAO 2 3.65- 9.39 4.44- 8.17 150 8-13 3 7.65-13.17 7.65-10.96 220,55 LRS 4 7.80-22.70 11.10-19.00 30 Engelke Fn. 5 1.25-35.00 19.10-35.00 -- References: 1. Strecker, Erickson, and Witteborn 1979, Ap.J. Suppl, 41, 501. 2. NASA-Ames KAO data from May 11, 1992 (alp Boo cf. alp Lyr) flight 3. NASA-Ames Mt. Lemmon data of Feb. 24, 1992 (alp Boo cf. alp Lyr) & UKIRT data of May 24 & 25, 1991 (CGS3 data of M. J. Barlow, priv. comm. to MC; alp Boo cf. bet Peg). 4. LRS raw data extracted from the new Groningen IRAS database and recalibrated with "LRSCAL" routine in "GIPSY" package. 5. Engelke Fn. used for T=4362K (see Blackwell, Lynas-Gray, and Petford 1991, A\&A, 245, 567) and angular diameter=20.430 mas; we rescaled this to 20.80 mas. This Engelke Function was locked to the photometrically scaled combination of 8-13 and LRS spectra by splicing and used to replace the observations beyond 19.10 um. A conservative error of 6.0% in EFn. due to effective temperature uncertainty was input for this fragment. Information on splices and biases incurred Process Factor determined +/-Bias% NIR cf. photometry 1.002 0.89 813 cf. photometry 1.056 0.85 LRS blue/red bias -- 0.03 LRS splice to 813 0.933 0.03 KAO joint splice to NIR and merged 813/LRS 0.850 0.32 Engelke Fn. splice to combined 813/LRS 1.037 0.26 ==================================================== Notes: 1. Template spectra are NOT tabulated at equal intervals of the wavelength, but rather at the wavelengths of the original measurements. 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. ====================================================