Throughout “Ice and Stone 2020” we have primarily been concerned with the objects we call “comets” and the objects we call “asteroids,” which collectively are “planetesimals” left over from the formation of the solar system. From an observational perspective, “asteroids” are stellar in appearance whereas “comets” are diffuse and fuzzy, while from a physical perspective “asteroids” are primarily made up of metals and silicate materials whereas “comets” are primarily made up of “volatile” substances like ices of water and gases like carbon monoxide and carbon dioxide. As is often true in many facets of nature, there is no clear dividing line between what constitutes an “asteroid” versus what constitutes a “comet,” and as was discussed in the “Special Topics” presentation five weeks ago, many apparent asteroids may in fact be “extinct” comets. There are quite a few other objects that exhibit characteristics of both comets and asteroids, and the issue of what to call them sometimes comes down to what they were called when they were first discovered.
One of the earliest examples of such a “dual-natured” object was discovered on November 19, 1949, by Albert Wilson and Robert Harrington during the course of the first Palomar Observatory Sky Survey conducted with the 1.2-meter Schmidt telescope. On both the blue- and the red-sensitive photographic plates it exhibited a distinct comet-like tail, although it did not exhibit a coma. Unfortunately, it was only photographed on three additional nights over the course of the subsequent week, and at best exhibited only a marginal cometary appearance on those photographs. There was not enough data to compute a valid orbit, with only a preliminary parabolic orbit being entered into the orbit catalogs, although the general consensus was that “Comet Wilson-Harrington” was very probably a short-period object.
There the matter stood until 1992 when Ed Bowell at the Lowell Observatory in Arizona was engaged in a project to find pre-discovery images of currently-known near-Earth asteroids on Palomar Sky Survey photographs. One of these was an object that had been discovered in November 1979 by Eleanor Helin with the 46-cm Schmidt telescope at Palomar, which had passed 0.09 AU from Earth three weeks earlier and which, after being recovered in 1988, had been assigned the asteroidal number (4015). The Sky Survey images of this object that Bowell identified were seen to show a cometary tail, which Brian Marsden at the IAU’s Minor Planet Center recognized as being none other than the “lost” “Comet Wilson-Harrington.” It turns out to have an orbital period of 4.3 years, a perihelion distance of almost exactly 1.0 AU, and an eccentricity of 0.62. As indicative of its “dual nature” the object was later assigned the short-period comet number 107P, and its “cometary” name and its “asteroidal” name are both Wilson-Harrington.
Wilson-Harrington appeared entirely asteroidal when it was re-discovered in 1979, and in fact with the exception of the photographs taken at the time of its original discovery in 1949 it has never exhibited any kind of cometary activity, although it has been carefully examined when circumstances have permitted it. The cause of the activity in 1949 remains a bit of a mystery, although a brief episode of cometary outgassing seems to be the most likely explanation. It will next pass somewhat close to Earth on October 31, 2039, when it will approach to slightly within 0.11 AU, and perhaps it will be amenable to detailed studies at that time.
One of the most interesting objects that illustrate the nebulous borderline between “asteroid” and “comet” was reported in early August 1996, when Eric Elst with the Royal Observatory in Uccle, Belgium found images of an apparent comet on photographs taken in mid-July by Guido Pizarro with the 1-meter Schmidt Telescope at the European Southern Observatory in Chile. The object, about 18th magnitude, did not show a coma but did exhibit a distinct tail several arcminutes long, which persisted for several weeks. It was found to be traveling in an orbit entirely typical of main-belt asteroids, i.e., an orbital period of 5.6 years, a perihelion distance of 2.63 AU, and a low eccentricity of 0.17, however in light of its persistent tail it was assigned both an asteroid number, (7968), and a short-period comet number, 133P, and the name Elst-Pizarro.
Elst-Pizarro had passed perihelion in April 1996 a few months before its discovery, however when it was recovered near opposition late the following year its appearance was completely stellar. Nevertheless, since that time it has exhibited a comet-like tail on several occasions around the times of subsequent perihelion passages, and thus it appears that Elst-Pizarro’s cometary activity is due to the sublimation of ices just as in the case of regular comets, but it happens to be traveling in an orbit more representative of main-belt asteroids.
Elst-Pizarro’s status as the only known “main-belt comet” changed in late 2005 when a second such object was discovered by Michael Read with the Spacewatch program in Arizona. At around that same time David Jewitt and Henry Hsieh at the University of Hawaii were engaged in a special search for cometary activity in asteroids when they detected a third such object, which had originally been discovered – as an “ordinary” main-belt asteroid – by the LINEAR program in New Mexico in late 1999. Since that time several more such objects have been discovered, and at least some of these have exhibited cometary activity on multiple occasions. It would appear, then, that these are genuine comets that reside permanently within the main asteroid belt.
It is conceivable that the population of “main-belt comets” is even larger than it currently appears. Based upon infrared observations obtained in 2009, the surface of the large main-belt asteroid (24) Themis appears to be almost entirely covered with water ice, although no evidence of sublimation of this ice has ever been detected. During recent years a team of Russian astronomers led by Vladimir Busarev has reported that some larger main-belt asteroids, including (145) Adeona, (704) Interamnia, and (779) Nina, have exhibited spectroscopic evidence for water ice sublimation, although so far none of these objects have shown direct physical evidence for such activity. Even the largest main-belt asteroid, (1) Ceres, has exhibited spectroscopic evidence for ice sublimation, and the Dawn spacecraft which has been in orbit around Ceres since early 2015 detected such evidence as well, although this was in the form of a temporary and extremely thin atmosphere that appears to be generated on occasion by strong solar activity.
Not all apparent cometary activity in asteroids can be attributed to water sublimation, however. A striking example is offered by the Apollo-type asteroid (3200) Phaethon, which was discovered by the InfraRed Astronomical Satellite (IRAS) spacecraft in October 1983 and found to be traveling in an elongated orbit with a period of 1.43 years and a perihelion distance of only 0.14 AU – the smallest for any asteroid known at that time. Fred Whipple soon pointed out that Phaethon has the same orbit as the Geminid meteor shower, and there has been a fairly strong consensus that Phaethon is indeed the parent object of the Geminids. It has made several relatively close approaches to Earth since that time, including one to 0.069 AU in December 2017, however, despite close scrutiny, it has never exhibited any cometary activity via ground-based observations.
Phaethon has nevertheless now shown cometary activity when close to perihelion passage when it is not observable from the ground. In June 2009 researchers noted that in near-sun images taken with the STEREO-A spacecraft it exhibited a coma and a tail-like extension, and it has done so again when near perihelion in 2012 and 2016. An analysis by David Jewitt and his colleagues at UCLA has demonstrated that these are indeed dust-ejection events, however, since any volatile substances that Phaethon might have possessed would have been cooked off by its repeated close passages by the sun, these events are likely due to sun-baked fracturing of its crust with the resulting dust then being swept off the surface due to solar radiation pressure. Phaethon could thus be described as a “rock comet” as opposed to a more conventional comet where the activity is driven by sublimation of ices. Jewitt and his colleagues have pointed out, incidentally, that the dust released from Phaethon during these episodes is too small by at least a factor of ten to account for the observed strength of the Geminid meteor shower, so it is entirely conceivable that it might have been a more conventional comet in the past.
Another interesting object is the Apollo-type asteroid (101955) Bennu, the current home of NASA’s OSIRIS-REx mission (discussed in last week’s “Special Topics” presentation). Between early January and mid-February 2019 – during which time Bennu was near perihelion – OSIRIS-REx detected eleven different plume ejection events of dust grains and larger particles off Bennu’s surface. While the complete explanation for this activity is perhaps not entirely certain at this time, various studies suggest that, while Bennu does appear to contain a non-trivial amount of water, the most likely causes of the activity are actually thermal fracturing of its surface (similar to, although smaller in scale than, the apparent cause of Phaethon’s activity) as well as meteoroid impacts, including ricochets from those impacts.
In January 2010 the LINEAR program in New Mexico discovered an apparent comet, originally designated as P/2010 A2, that appeared to consist entirely of a tail without an apparent “head.” Detailed studies afterward, including with the Hubble Space Telescope, showed a small apparent asteroid near the front end of this tail, although detached from it, and analysis indicates that we were witnessing the result of an impact between two small asteroids, with the “tail” being the debris field created from this event. The object was found to be traveling in a near-circular orbit in the inner portion of the main asteroid belt with a period of 3.5 years, and after being recovered (without any tail or other cometary features) in 2017 has nevertheless been assigned the cometary designation 354P/LINEAR.
An even more interesting event took place later in 2010 when on December 11 Steve Larson with the Catalina Sky Survey in Arizona reported that the large main-belt asteroid (596) Scheila, which had been discovered by the German astronomer August Kopff in February 1906 and which had been an “ordinary” asteroid ever since – was over a magnitude brighter than expected, and moreover was accompanied by an extended coma roughly 2 by 5 arcminutes across. This coma dispersed over the next few weeks, and a spectroscopic analysis indicated it was made up entirely of dust, i.e., there was no evidence of any gases present. Researchers concluded that the coma and overall outburst was caused by the impact of a small (35-meter) asteroid onto Scheila itself. A similar event seems to have occurred in early 2015, when on March 17 David Tholen, Scott Sheppard, and Chad Trujillo detected a faint comet-like tail extending from the large main-belt asteroid (493) Griseldis in images taken with the 8.2-meter Subaru Telescope at Mauna Kea. This feature, too, dispersed not too long thereafter and also appears to be due to an impact event. Neither Scheila nor Griseldis has exhibited any additional signs of cometary activity since their respective outbursts.
Another source of apparent cometary activity in asteroids is demonstrated by two “comets” discovered by the Hawaii-based Pan-STARRS program in 2013 (although other similar objects have also been discovered), P/2013 P5 and P/2013 R3 (the latter object being independently discovered by the Catalina Sky Survey in Arizona). Both objects were found to be spewing streams of dust by rapidly-rotating asteroids being spun up by sunlight via the Yarkovsky-O’Keefe-Radzievskii-Paddack (YORP) effect, which is caused by scattering of sunlight impinging on planetary surfaces and by emission of thermal radiation. Both objects travel in orbits typical of main-belt asteroids: P/2013 P5 is in a near-circular orbit in the inner asteroid belt with a period of 3.24 years and, having been observed as recently as 2018 and in fact, would have passed through perihelion again this past October, has been assigned the periodic comet designation 311P/PANSTARRS, while P/2013 R3, which traveled in a larger orbit with a period of 5.3 years, apparently completely disintegrated in early 2014 and has not been detected since then.
An interesting variation of the apparent YORP-effect driven cometary activity is provided by the main-belt “asteroid” (6478) Gault, which exhibited a distinct comet-like tail in late 2018 and early 2019. Although this does appear to be another example of a YORP-effect “comet,” a search of old images has revealed that Gault has exhibited this tail-like feature at least a far back as September 2013, suggesting there may be more to its story. Gault is a previous “Comet of the Week” and that overall story is discussed more completely in that presentation. For what it’s worth, Gault, which was at opposition back in late September, has not exhibited any unusual activity or appearance this year.
All of the objects described in this presentation illustrate that there is no firm distinction between a “comet” and an “asteroid,” and that there are quite a few objects that exhibit characteristics of both. Indeed, for a rather extreme example, sodium atoms from Mercury’s surface and its (very thin) atmosphere are pushed away by sunlight (in the same manner as dust grains are pushed away from cometary nuclei by sunlight), and in images taken with special filters that isolate the light of sodium atoms Mercury is accompanied by a distinct tail that gives it the superficial appearance of a comet. This phenomenon was predicted in the mid-1980s and was first detected in 2001.
For my own observational purposes, I consider any “small body” that has exhibited distinct physical cometary activity at some point, including objects like (596) Scheila and (493) Griseldis, as a “comet,” although I draw the (admittedly arbitrary) line at Mercury. Collectively, all of these objects illustrate that our solar system is a complex place, and each of the objects have their own unique story to tell.
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