On the Nature of the Anti-Tail of Comet Kohoutek (1973F)
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zcAavs 27, 135-146 (1976) On the Nature of the Anti-Tail of Comet Kohoutek (1973f). I1. Comparison of the Working Model with Ground-Based Photographic Observations ZDENEK SEKANINA Center for Astrophysics, Harvard College Observatory and Smithsonian Astrophysical Observatory, Cambridge, Massachusetts 02138 AND FREEMAN D. MILLER Department of Astronomy, University of Michigan, Ann Arbor, Michigan 48104 Received May 13, 1975; revised June 3, 1975 Photographic observations of the anti- tail of Comet Kohoutek ( 1973f ), obtaitled at the Cerro Tololo Inter-American Observatory, are photometrically reduced and the results compared with a recently formulated working model of the anti- tail. The applied technique of photometric reduction is described, and the radial and transverse profiles of the anti-tail, corrected for the effects of atmospheric extinction and the variable intensity of the ambient sky, are derived. Brightness variations in time are also studied, The most important result reached so far is a quantitative confirmation of the previously suggested hypothesis, arguing that dust particles in the anti-tail suffered a significant loss in radius due to evaporation near the perihelion passage. We find that only particles initially larger than 100-150/~m in diameter (at an assumed density of I gcm -3) survived. Numerically, however, this result is still preliminary, because the dynamical effect associated with particle evaporation remains to be explained. It is also tentatively suggested that. the emission rate of the dust from the comet was probably comparable with the rates derived earlier for Comets Arend-Roland (1957 III) and Bennett (1970 II). I. INTRODUCTION then tested quantitatively. The photo- graphic material studied here was secured A working model was recently formu- under the supervision of the second author. lated for the anti-tail of Comet Kohoutek The photometric reduction and physical (Sekanina, 1974; referred to hereafter as interpretation are due to the first author. Paper I). The model was based on the Finson-Probstein (1968) theory of dust II. TttE MICHIGAN PROGRAM OF comets and fitted reasonably well the semi- PHOTOGRAPHIC OBSERVATIONS OF COMETS quantitative descriptions of the anti-tail by a number of observers, including the The plates described in Section III form Skylab III astronauts. In the present paper, part of a program of comet observations the radial and transverse brightness pro- initiated by the second author in 1950 with files and the time variations in the surface the Curtis-Schmidt telescope (61/91cm, brightness of the anti-tail are established f/3.5, 96':6mm -~) of the University of from plates of the comet taken at the Cerro Michigan. ]in addition to unfiltered "blue" Tololo Inter-American Observatory, near plates, exposures have been taken through La Serena, Chile, and the working model is red filters to suppress the CO t emissions of Copyright (c) 1976 by Academic Press, Inc. 135 All rights of reproduction in any form reserved. Printed in Great Britain 136 SEKANINA AND MILLER Type I tails relative to the scattered Still- telescope between January 16 and Feb- light of the Type II tails, on which the ruary 15, 1974. Five plates, taken on former are often superposed. The extent to January 23, 24, and 26 and February 12 which the suppression is successful has and 15, are 098-02 panchromatic enmlsions varied from one comet to another (Miller, combined with an RG1 filter to provide 1958, 1962). The development of a model maximum sensitivity near 661~(1A and of dust tails by Finson and Probstein (1968) to cut off the visible spectrum below has stimulated interest in the study of the A ~ 5900A. The photometric system thus Michigan material, and analyses for Comets obtained is similar to the R system of Seki-Lines 1962 III (Jambor, 19731 and Johnson and Mitchell (1962). The other Bennett 1970 I] (Sekanina and Miller, seven plates, taken on January 16, 17, 20, 1973) have already appeared. 21, 23, 25, and 27, are standard 103a-O From the first, the comet-program plates emulsions without filter. The red-sensitive have been photometrically calibrated with plates are of primary interest, both a 14-tube spot sensitometer designed by because they span a longer interval of E. B. Weston; when the telescope was time and because they show the anti-tail transferred from Michigan to Cerro Tololo, better. The guiding of the ,lanuary 24 the sensitometer accompanied it. Since the plate was somewhat imperfect, so only the precision of the sensitometer calibration is other four plates, two in January an(I two critical, the photometric scale was meas- in February, have been photometricall.v ured photoelectrically by W. Liller in 1951 studied. The four observations are listed and 1955 and by S. M. Simkin in 1965. The in Table 1. average deviation from the mean scale of Of much concern has been the very low the three independent measurements for altitude of the comet. At the end of the each spot is ±0.04mag; a more detailed exposure, the comet was only slightly over discussion of the calibration tests can be 1() ° above the horizon on plates 15520, tbund in a paper by Miller (1967). A calibra- 15687, and 157(i13 and about 7 ° above the tion exposure is made for each comet horizon on 15554! Thanks to the excellent photograph through the same filter used in sky at Cerro Tololo, the plates are still the comet exposure and on a plate taken photometrically valuable, but the very from the same box and developed with the low altitude of the comet is a source of two comet [)late. The length of the calibration potential complications for the photometry exposure is the same as that, for the comet. of the plates, namely the effects of dif- ferential refi'action and strongly variable sky brightness. In addition, atmospheric III. THE (~ERRO TOLOLO PHOTOGRAPHS extinction, which is severe at these alti- A total of 12 calibrated plates were taken tudes even in the red section of the at Cerro Tololo with the Curtis-Schmidt spectrum, also needs to be accounted for. TABLE I (~ERRO TOLOLO ]~E|)-SENSITIVE PHOTOGfCAPHS OF (~OMET ]%OHOUTEK (098-02 EMULSION "tVITHAN RGI FILTEU) C,omet's posit, ion 1950.0 Phas(' Date UT /1 r angle Altitude at Exl)oSur(~ Platte 1974 R.A. I)eel. (AU) (AU) ~ midexposure" (mm) 15520 Jan. 23.0495 23n40~. 67 +@ 46~5 O.853 O.837 71 ~2 1316 20 15554 Jan. 26.0614 0n07 .m3(~ +3c 12:2 0.894 (k909 66.2 I 1~8 50 15687 Feb. 12.0572 lh54m21 +12~01:9 1.257 1.278 45 ~ 16~3 60 15703 Feb. 15.0566 2h07T40 +12 57~7 1.334 1.338 43'14 16~2 60 " Not corrected tbr t~ depressed horizon. THE ANTI-TAIL OF COMET KOHOUTEK (1973f). II 137 The differential-refraction effect has been quantitatively analyzed following the procedure described in Appendix A. PLATE 15 Numerically, refraction has been found to affect the angular distance from the nucleus on the four plates by less than 1%, and the position angle, by no more than 0.1 ° at an angular distance of 1 ° from the nucleus and no more than 0.2 ° at 2 +. The effect of variable sky brightness proved considerably more severe. It so happened that the brightest section of the anti-tail was directed almost exactly toward the horizon on all the plates, so that the maximum brightness gradient of the sky projected unforeshortened along the anti-tuil. In addition, all exposures began during astronomical twilight (with the Sun's depression between 15 + and 17°), and almost the whole 15520 exposure was taken during twilight (with the Sun's depression at midexposure 17+). To demon- strate the extent of interference, we I000 mention that the relative gradient of the sky brightness on plates 15520 nad 15554 /• reached a maximum rate of 7% per degree S(;~,LE of altitude, while at the same time the intrinsic surface brightness of the anti-tail 0 I0' 20 ~ 50 / Fro. 1. A two-dimensional scan of plate 15687. amounted to only some 4-6% of the sky Scanning aperture is 9'.'7 by 9'.'7. The anti-tail brightness at 15' from the nucleus and points to the bottom of the scan, and the regular about 1-2% at 25". dust tail to the top. The numbers indicate the relative surface brightness, uncorrected for the contribution from the sky. IV. THE TECHNIQUE OF PHOTOMETRIC REDUCTION known positions have been used to fix the The technique for reducing the plates position angles. The position of the comet was essentially dictated by the trouble- on the plates was measured relative to the some observing conditions. Because of the ambient stars and reduced routinely with complicated character of the sky-bright- the use of the method of dependences. The ness variations near the horizon, it was result has also been checked by computing virtually impossible to use the standard the expected topocentric position of the two-dimensional scans to map the sky comet from Marsden's (1974) definitive "noise" over the area occupied by the orbit. The measured and computed posi- anti-tail (see Fig. 1). Preferable, because tions agree within 2" on plate 15520, more revealing, are one-dimensional radial 7" on 15554, 8" on 15687, and 13" on 15703. tracings, passing through the comet's These residuals can be accounted for nucleus and effectively covering the whole entirely by the uncertainty in the location anti-tail. Each radial scan is defined by on the plates of the nucleus in the strongly the position angle, and the "noise" varia- overexposed coma, which is almost 2' in tions in the respective section of the anti- diameter.