The light curve of periodic comet Halley 1910 II

1982 ◽  
Vol 87 ◽  
pp. 918 ◽  
Author(s):  
C. S. Morris ◽  
D. W. E. Green

1989 ◽  
Vol 116 (1) ◽  
pp. 175-207
Author(s):  
Imke de Pater ◽  
Patrick Palmer ◽  
Lewis E. Snyder

AbstractWe present an overview of cometary observations carried out with the VLA. These include OH imaging observations, studies of other molecules and searches for continuum emission. Primarily, we discuss the OH observations obtained of Comet Halley, a periodic comet, and Comet Wilson, a “new” comet. The emission from Comet Halley is confined to a region a few times 105 km. The emission from Comet Wilson shows sporadic blobs at large distances (∼ 106 km from the center), which vary abruptly in both position and velocity. The generally accepted picture of excitation by UV pumping in a spherical outflow of cometary gas explains the coarse phenomenology, but other effects seem to cause significant modulations of the OH emission. We suggest that for Comet Halley, collisional effects near the edge of the quenching region, which is coincidently the approximate distance to the cometopause, may be important, and that for Comet Wilson, outgassing from cometesimals ejected from the nucleus may be significant. We further show that asymmetric line profiles are more common than previously thought. Lengthening integration times and lowering the velocity resolution results in a smooth, round shape for the comet’s brightness distribution. In addition, spectral profiles become broader and more symmetric after long integration times and after integration over larger spatial regions. In addition to the OH observations we summarize the H2CO detection experiments for comets Halley and Machholz.



1989 ◽  
Vol 45 (1) ◽  
pp. 17-27 ◽  
Author(s):  
P. S. Goraya ◽  
B. S. Rautela ◽  
B. B. Sanwal ◽  
S. K. Gupta ◽  
H. K. Duggal ◽  
...  


Two kinds of smaller bodies in the Solar System, the minor planets and the comets, are of interest from the point of view of space exploration and of our System's origin; of these the comets are, for the decade that has just begun, without any doubt by far the more important ones. One of the reasons is purely accidental: the return of comet Halley in 1985-86. Being the only case on record of a periodic comet that has remained an easy naked-eye object after some dozen returns, it provides opportunities for in situ studies also, during a fast fly-by mission, which are unlikely to occur again for many years to come. Another reason is that, according to the conviction of almost all workers in the field (cf. the last tri-annual Reports of I.A.U. Commission 15), the comets are among the most pristine objects in the Solar System and most probably closer to the original state than is any other. New insights into their origin have revived the suggestion which had been made already 6 or 7 years ago, that they did not originate in the presolar nebula (ps.n.) itself, but in a satellite nebula or in other nearby fragments of the same parent interstellar cloud, providing another way by which material of a somewhat different early history might have been added to that of the planetary system (Cameron 1973; Biermann 1979). It is my intention to develop this aspect in some more detail.



1974 ◽  
Vol 22 ◽  
pp. 307 ◽  
Author(s):  
Zdenek Sekanina

AbstractIt is suggested that the outbursts of Periodic Comet Schwassmann-Wachmann 1 are triggered by impacts of interplanetary boulders on the surface of the comet’s nucleus. The existence of a cloud of such boulders in interplanetary space was predicted by Harwit (1967). We have used the hypothesis to calculate the characteristics of the outbursts – such as their mean rate, optically important dimensions of ejected debris, expansion velocity of the ejecta, maximum diameter of the expanding cloud before it fades out, and the magnitude of the accompanying orbital impulse – and found them reasonably consistent with observations, if the solid constituent of the comet is assumed in the form of a porous matrix of lowstrength meteoric material. A Monte Carlo method was applied to simulate the distributions of impacts, their directions and impact velocities.



1997 ◽  
Vol 161 ◽  
pp. 179-187
Author(s):  
Clifford N. Matthews ◽  
Rose A. Pesce-Rodriguez ◽  
Shirley A. Liebman

AbstractHydrogen cyanide polymers – heterogeneous solids ranging in color from yellow to orange to brown to black – may be among the organic macromolecules most readily formed within the Solar System. The non-volatile black crust of comet Halley, for example, as well as the extensive orangebrown streaks in the atmosphere of Jupiter, might consist largely of such polymers synthesized from HCN formed by photolysis of methane and ammonia, the color observed depending on the concentration of HCN involved. Laboratory studies of these ubiquitous compounds point to the presence of polyamidine structures synthesized directly from hydrogen cyanide. These would be converted by water to polypeptides which can be further hydrolyzed to α-amino acids. Black polymers and multimers with conjugated ladder structures derived from HCN could also be formed and might well be the source of the many nitrogen heterocycles, adenine included, observed after pyrolysis. The dark brown color arising from the impacts of comet P/Shoemaker-Levy 9 on Jupiter might therefore be mainly caused by the presence of HCN polymers, whether originally present, deposited by the impactor or synthesized directly from HCN. Spectroscopic detection of these predicted macromolecules and their hydrolytic and pyrolytic by-products would strengthen significantly the hypothesis that cyanide polymerization is a preferred pathway for prebiotic and extraterrestrial chemistry.



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