Circular No. 4620 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 617-495-7244/7440/7444 MARSDEN or GREEN@CFA.BITNET MARSDEN or GREEN@CFAPS2.SPAN NOVA ANDROMEDAE 1988 Information received some weeks ago indicates that a spectrogram was obtained of D. McAdam's variable in Andromeda (IAUC 4570, 4577, 4579) with the 2.5-m Isaac Newton Telescope, La Palma, on Apr. 1, but various computer problems have prevented recovery of the data. A preliminary inspection of the object's spectrum at the time apparently showed the presence of strong O III emission. Referring to the measurements of the position of the object (IAUC 4577), G. M. Hurst, Basingstoke, England, reports that B. Manning, Stakenbridge, has obtained the following position (a three-star SAOC reduction from a Palomar Sky Survey print) for Hurst's pre-outburst candidate: R.A. = 2h26m22s.18, Decl. = +39D49'17".4 (equinox 1950.0). No image appears on the Franklin-Adams chart (1908 Dec. 28) to mag 15. Further visual magnitude estimates: Apr 11.85 UT, 12.2 (Hurst); 12.84, 12.3 (Hurst); 12.86, 12.3 (S. Lubbock, Bridgend, Wales); 13.86, 12.5 (Lubbock). A 12-min exposure (0.57-m reflector, K2415 film) by A. Young, Burwash, on June 23.04 UT failed to record the object to a limiting magnitude of about 16.0. Although the absence of more definite observations is unfortunate, it seems reasonable to suppose that the object was a nova. OCCULTATION BY PLUTO W. S. G. Walker, D. Dix, B. F. Marino and G. Urquhart, Auckland Observatory, refine their timings of the June 9 occultation (IAUC 4612) as follows: atmospheric ingress, 10h37m48s.8 UT; planetary ingress, 10h38m12s.8; planetary egress, 10h39m51s.3; atmospheric egress, 10h40m12s.8. They add: "The relative times are reliable, but the absolute times are uncertain by +/- 2 s. Cloudy weather precluded a final test of the high-speed data-acquisition system before the event. The ingress contains three distinct slopes, indicative of layering in the atmosphere. These slopes are less discernible in the egress because of a minor system problem. The atmospheric ingress and egress differ in slope and duration, presumably indicating some tidal distortion in the direction of Charon." SUPERNOVA 1988A IN M58 Corrigendum. On IAUC 4613, line 10, for B-V = +0.7 read B-V = +1.3. 1988 July 1 (4620) Brian G. Marsden
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