COMMISSIONS 27 AND 42 OF THE IAU INFORMATION BULLETIN ON VARIABLE STARS Number 3853 Konkoly Observatory Budapest 2 March 1993 HU ISSN 0374-0676 TIME OF LIGHT MINIMUM OF BW VULPECULAE^1 BW Vul (HD 199140 = HR 8007, B2III, V = 6.55) has the largest known amplitude of light variation and radial velocity variation among the beta Cephei stars. The period of the variation is approximately 5h, and is now increasing at a rate of about 2 seconds/century. We report photometric observations obtained on September 26, 1992 at Jungfraujoch Observatory with a 76 cm reflector telescope and the Geneva P1 photoelectric photometer. A Lallemand S-11 photomultiplier, refrigerated at about -23degC, was used as detector. The system was equipped with a DC amplifier and a strip-chart recorder. All measurements were taken through the V, filter of the Geneva system. Comparison stars were the same as C_1 and C_2 used by Sterken et al. (1986), viz. HD 198820 = HR 7996 (B3III, V = 6.44) and HD 198527 = SAO 089185 (B9.5V, V = 7.0). The observations were carried out recording to the scheme C_1, BW Vul, C_1, BW Vul, C_1, BW Vul ... and, in addition, a measurement of C_2 was taken at the beginning and at the end of the complete observing sequence. Each datapoint consisted of a measurement of about 1 minute duration. Sky background was measured about once every two cycles. The data were corrected for sky background contribution, and for the effect of atmospheric extinction; the extinction coefficient kv_1 = 0.569 was derived by application of the classical Bouguer method on the measurements of C_1. The mean magnitude difference between C_1 and C_2 (in the sense C_1 minus C_2) was -0.754 +- 0.003m. Considering the rather large value for the extinction coefficient, and also the fact that the measurements had to be stopped for cirrus clouds, we assess the quality of our data as of weight 2-3 on the scale given by Sterken et al. (1993). Table 1 gives the differential V1 magnitudes BW Vul minus C_1 The time of minimum light Tmin = HJD2448892.3949 was derived using the method outlined by Sterken et al. (1987). The residual to the linear ephemeris given by Sterken et al. (1993) equals -0.0038d. Figure 1 shows all Tmin values obtained since June 15, 1988 (that is, our new Tmin and also those taken from Table 1 of Sterken 1993). Our result indicates that probably no abrupt change in the period of BW Vul has occurred in the last year. However, more photometric data are needed to elucidate how much of the forthcoming changes of the period of BW Vul can be ascribed to the light-time effect in a binary system. For a detailed discussion on the interpretation of the period changes in BW Vul, we refer to Sterken (1993). [FIGURE 1] Figure 1: O-C diagram for all available times of minimum since June 15, 1988 (the solid circle represents the new time of minimum reported in this paper) according to the cycle-count scheme given by Sterken (1993) and with P=0.2010443d and T0=2447328.4751d. Table 1. Differential V_1 magnitudes of BW Vul minus HD 198820. HJD is heliocentric julian date minus 2,440,000. HJD Delta V_1 HJD Delta V_2 8892.3482 0.130 8892.3602 0.169 8892.3644 0.201 8892.3686 0.209 8892.3779 0.228 8892.3818 0.221 8892.3866 0.233 8892.3906 0.229 8892.3946 0.234 8892.3984 0.232 8892.4028 0.225 8892.4087 0.222 8892.4130 0.218 8892.4182 0.216 8892.4224 0.198 8892.4262 0.192 8892.4302 0.189 8892.4339 0.160 8892.4375 0.153 8892.4412 0.133 This work was supported by a research grant from the Belgian Fund for Scientific Research (NFWO). C. STERKEN (National Fund for Scientific Research) University of Brussels Pleinlaan 2, B-1050 Brussel Belgium References: Sterken C., Snowden M., et al., 1986, Astron. Astrophys. Suppl. Ser., 66, 11 [BIBCODE 1986A&AS...66...11S ] Sterken C., Young A., and Furenlid I., 1987, Astron. Astrophys., 177, 150 [BIBCODE 1987A&A...177..150S ] Sterken, C., Pigulski, A., and Liu Zongli; 1993; Astron. Astrophys. Suppl. Ser., in press [BIBCODE 1993A&AS...98..383S ] Sterken C., 1993, Astron. Astrophys., in press [BIBCODE 1993A&A...270..259S ] ^1 BASED ON OBSERVATIONS COLLECTED AT THE HOCHALPINE FORSCHUNGSSTATION JUNGFRAUJOCH (SWITZERLAND)