Circular No. 3527 Central Bureau for Astronomical Telegrams INTERNATIONAL ASTRONOMICAL UNION Postal Address: Central Bureau for Astronomical Telegrams Smithsonian Astrophysical Observatory, Cambridge, MA 02138, U.S.A. TWX 710-320-6842 ASTROGRAM CAM Telephone 617-864-5758 A0535+262 N. Oda and the Hakucho Team, Institute of Space and Aeronautical Science, University of Tokyo, report: "The x-ray nova discovered with the y-axis scanning detectors of Hakucho on Oct. 2 (cf. IAUC 3525) was confirmed to be A0535+262. Since Oct. 10, z-axis detectors have been watching the source, and the error circle for the source location was refined to be 0o.5 in radius centered at the position of A0535+262. Typical 104-s x-ray pulsation was also observed. The intensity is ~ 0.7 Crab (1-10 keV) as of Oct. 12." SS 433 T. Mazeh, E. N. Leibowitz, O. Lahav and Y. Sheffer, Wise Observatory, telex: "Fifty-four nightly averages of the V-magnitude of SS 433, measured between 1979 July and Oct., and 23 averages measured between 1980 Nay and Sept., indicate a photometric period of 6d.36 +/- 0d.08. The amplitude of the systematic variation is 0.3 mag (cf. Kemp and Barbour, IAUC 3484). The B-V index shows no dependence upon the phase of this periodicity." (201) PENELOPE J. Surdej, Institut d'Astrophysique de Liege and European Southern Observatory; and N. Cramer, Observatoire de Geneve, communicate: "UBV photometry with the ESO 5-m telescope and seven-color photometry with the Geneva 7-m telescope were performed for (201) Penelope at La Silla on Oct. 6, 11 and 17, and Oct. 8 and 14, respectively. This minor planet is found to have a rotation period of 3h45m30s +/- 18s (see also IAUC 3523), and its lightcurve displays two distinct maxima and minima with a total amplitude V ~ 0.52 mag The color indices B-V (~ +0.70) and U-B (~ +0.23) show noticeable variations (0.05 and 0.06 mag, respectively) during a single period. Furthermore, there appear to be shifts iin phase between the V, B-V and U-B measurements reaching ~40 min at some points of the lightcurve. These results have been confirmed at each run of observations. Whereas large albedo variations over the surface of this object are probably responsible for the interesting observed features, other causes cannot be entirely excluded. Further observations (photometry, infrared, spectrophotometry, polarimetry, etc.) are highly desirable." 1980 October 20 (3527) Daniel W. E. Green
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