THE ASTROPHYSICAL JOURNAL, 461:L119[–]L122, 1996 April 20
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Evolution of a Spiral Jet in the Inner Coma of Comet Hale-Bopp (1995 O1)
Mark R. Kidger, Miquel Serra-Ricart, Luis R. Bellot-Rubio, and Ricard Casas
Instituto de Astrofísica de Canarias, Via Lactea E-38200 La Laguna,
Tenerife, Canary Islands, Spain; mrk@iac.es; mserra@iac.es; lbellot@iac.es;
rcr@iac.es
Received 1995 September 7; accepted 1995 December 6
ABSTRACT
We present observations of the evolution of a prominent spiral jet in
the inner coma of comet Hale-Bopp (1995 O1). The observations, taken with
the 82 cm IAC-80 telescope at the Teide Observatory, were made on 1995
August 25, 27, 28, and 31, and on September 4[–]7, as part of an
ongoing program of monitoring the comet in Tenerife. The jet is observed to
show a nearly, but not completely, constant position angle over the two
weeks of observation. Although it is generally assumed that the jet is a
dust event, some aspects of the morphology and behavior mean that the
hypothesis that it is a gas jet cannot be ruled out. No single hypothesis
is thought to be completely satisfactory. Between our first detection of
the jet on August 25 and its disappearance on September 7, we see the point
of inflection within the jet expand away from the nucleus at a highly
constant velocity. At the same time, the jet fades considerably. This jet
event seems different from others that have been observed later because the
collimation of the beam is very tight, rather than the highly wound spiral
structure shown by some later jets.
Subject headings: comets: individual (Hale-Bopp 1995 O1)
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CONTENTS
* 1. INTRODUCTION
* 2. OBSERVATIONS
* 3. RESULTS
* 4. DISCUSSION
* 5. CONCLUSIONS
* ACKNOWLEDGMENTS
* REFERENCES
* FIGURES
* TABLES
* REFERENCES TO THIS ARTICLE
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§1. INTRODUCTION
Comet Hale-Bopp was discovered visually by A. Hale and T. Bopp (Hale &
Bopp 1995) on 1995 July 23 at the unprecedented distance of 7.3 AU from the
Sun, by far the greatest distance for a visual comet discovery, and unusual
even for photographic or CCD discoveries. Since the comet exhibits a very
bright total visual magnitude at discovery, it is evident that it is either
particularly large and/or active or is suffering an exceptional outburst.
Despite the announcement of various prediscovery images of the comet, the
very sparse coverage that they offer and the doubts expressed about some of
these images mean that it is still not obvious whether comet Hale-Bopp is a
giant object showing its [“]normal[”] activity or a rather
smaller object showing an outburst. As a consequence, there is a range of
at least 10 mag between the best and the worst cases in the extrapolation
of its light curve to perihelion (Kidger 1995). One way of distinguishing
between scenarios is to establish the comet's degree and pattern of
activity. A high and stable degree of observed activity, combined with a
consistently bright total magnitude, would indicate that the more
optimistic predictions about the light-curve evolution may be correct. In
contrast, single-vent activity (from a lone active zone) would be a warning
sign that the comet may not fulfill the more optimistic predictions, even
fading out before perihelion.
Indirect evidence, such as the multiple similarities to comet 1811 I
(the orbit, very bright absolute magnitude, and activity at high
heliocentric distance), has been used (Marsden 1995) to suggest that comet
Hale-Bopp may be similarly spectacular near perihelion, although there is
little strong physical evidence that exists to support either of the
extreme scenarios (very bright or fizzle). Jet activity at high
heliocentric distance, though, is potentially a good indicator of the
intrinsic activity of the comet. No really bright object has been observed
since comet West in 1976, hence, the apparition of a potentially magnitude
zero (or brighter) comet, which will be well positioned to observe from the
northern hemisphere for several months around perihelion, is of great
interest for cometary physics. The fact that the comet is still 18 months
from perihelion allows detailed observing plans to be made. The advances in
astronomical instrumentation since 1986 will allow detailed spectroscopic
and morphological studies to be made that have never previously been
possible, especially if the comet is particularly bright.
Reports were made soon after the discovery of unusual activity (Offut
1995) with a spiral coma developing and decaying. This has been interpreted
as outburst activity similar to comet P/Schwassmann-Wachmann 1 (Sekanina
1995a). Such activity allows, in principle, the rotation period of the
nucleus to be estimated from the change in position angle of the jet (for
gaseous events), or from the synchrone trajectory (for dusty events). To
date, very few comets have a really well-determined rotation curve, and,
even in the case of P/Halley (the best observed object), the presence of
both 50 hr and 7 day periods means that there is no real consensus as to
the exact mode of rotation and precession around the long and short axes of
the nucleus.
§2. OBSERVATIONS
Regular observations of comet Hale-Bopp were started on August 10
using the CCD camera of the 82 cm IAC-80 telescope sited in Instituto de
Astrofísica de Canarias's Teide Observatory, Tenerife, Canary Islands,
Spain. A Thomson 1024 × 1024 chip was used, offering a field of nearly 7
[&farcm;]5. Standard BVRI broadband filters were used.
Because of the movement of the comet and the inability of the
telescope at present to track differentially, comparatively short exposures
are taken (each of 300[–]400 s), which are then recentered on the
cometary nucleus and summed to give any desired total exposure. The
position of the nuclear condensation was measured using the imexamine
routine, and images were combined using the imcombine routine, both
included in the Image Reduction and Analysis Facility (IRAF) 1 environment.
Images were previously flat fielded using very high S/N master dome flat
fields obtained by combining many individual exposures.
On some nights exposures were taken in all four filters to give color
information, but, on the eight nights to be discussed here, many exposures
were taken in a single filter, with the aim of combining them into a very
deep image in a single band. On discovering the jet, our observing program
switched to intensive monitoring in a single band on each night, to follow
the jet evolution with time. The observing log for the eight nights in
question is given in Table 1.
FOOTNOTES
1 IRAF is distributed by the National Optical Astronomy Observatories,
which is operated by the Association of Universities for Research in
Astronomy, Inc. (AURA), under cooperative agreement with the National
Science Foundation.
§3. RESULTS
On-line visual inspection of the images from August 28 revealed an
unusual jet emanating from the nucleus in P.A. = 280°. This jet wrapped
around the nucleus to P.A. = 030° approximately. The jet was also detected
by Jewitt & Chen (1995) some 9 hr after the start of observations from
Teide Observatory. On inspection of images from previous nights, the jet
was found to be very obviously present when the images were scaled
logarithmically to show the central condensation, rather than being scaled
to show the extended coma.
On August 25, the jet was significantly less extended in position
angle than on August 28, being clearly detected only to P.A. = 000°
approximately. The observations on August 27 were taken through an
occasionally dense cirrus cloud, which much reduced their quality. Even so,
the jet can be clearly traced from the nuclear condensation to P.A. = 020°
approximately, rather less than the observed extension on August 28, but
consistent with the poorer conditions.
To investigate the possible rotation of the jet, the images from each
night were grouped to give high S/N master frames. The images from August
25 and 28 were split initially into three sets of seven or eight frames,
recentered and combined. All the usable images from August 27 were combined
into a single frame. This frame was first smoothed slightly with a low-pass
Gaussian filter, and then a Laplacian filter was applied, leaving just the
jet and inner part of the central condensation visible. The combined and
recentered frames were then converted to MPEG format and animated (not
shown here, but available at http://www.ll.iac.es/general/index.html) to
show the evolution of the jet visually and dynamically. For the purposes of
this paper, though, all images from a single night have been combined,
given that we can rule out the existence of a significant rotation within a
single observing run. Figures 1(a)[–]1(e) (Plates L21[–]L25)
show the final reduced images for the nights when the jet is most clearly
seen. From September 4, the visibility was greatly reduced, partly by the
reduction in surface brightness and partly by the proximity of the Moon.
The jet is seen to have a three-part structure: there is an initial narrow
straight jet of material [∼]7[&arcsec;] long and gradually increasing
with date, leaving the nucleus in P.A. [∼] 280°. This straight section
appears to be highly collimated and has negligible curvature. This we refer
to as [“]the collimated jet.[”] This section abruptly changes
direction by 90° and opens out at a comparatively narrow opening angle
before starting to sweep round to the east and opening out further. Similar
behavior was reported by West (1995), who also observed the jet on several
nights, confirming the position angle of the collimated jet and its
constancy.
[Image] [Image] [Image] [Image] [Image] Fig. 1
Considerable differences are seen in the structure of the jet between
August 25 and 31. Apart from the extent of the jet in position angle, it is
seen to be wider and much brighter on the former date. The initial
collimated section of the jet increases slowly in length as it fades. We
cannot rule out, though, that there is a small oscillation in position
angle, although this appears to be less than [∼]15° and of indefinite
period. There is, though, no significant rotation of the jet on timescales
of either a few hours or a few days. We also note that the position angle
given by Jewitt & Chen (1995), observing from 7[–]9 hr after us on
August 26, was also 280°.
The end of the jet increases its distance considerably from the
nucleus, giving the false impression of rotation because it is
[“]unwinding.[”] On August 31 and September 4, the trend of a
gradual fade and pronounced increase in distance of the [“]spiral arm
[”] from the nucleus continues. After September 4, precise
measurements of the jet are extremely difficult due to its faintness. On
various nights, the data taken were nonphotometric or of dubious
photometric quality. This makes it difficult for us to quantify the rate of
fade of the jet, a potentially powerful diagnostic tool of its composition.
We are unable to say exactly when the jet appeared. There is no sign
of it in the images from August 15, which we include for comparison to show
that there are no important artifacts created by our reduction procedure.
From the rate of growth of the jet, we estimate that it took several days
before our first detection. Various reports on the Internet from reliable
visual observers speak of a sharp brightening of the nuclear condensation
of the comet around August 20, consistent with the initiation of an
outburst. Figure 2 shows the growth of the linear section of the jet during
the observations. A highly linear expansion is seen, with a projected
velocity of 32 m s-1, which cuts the x-axis at -7.69 days (August 17.31);
although there is no strong reason why this should be the actual date of
initiation of the structure.
[Image] Fig. 2
§4. DISCUSSION
The most popular explanation presented to date is that the jet is a
pure dust event, caused probably by CO sublimation, and that the curvature
reflects synchrone trajectories of grains of very different sizes. If the
jet is caused primarily by dust (or ice) and neutral gas ejection, no
rotation in position angle would be seen, although the morphology of the
jet would reveal the rotation period and axial inclination. This
explanation is favored by various authors (e.g., Sekanina 1995b, c).
To obtain a good fit to the jet morphology, some very tight
constraints are made on models. It is necessary to suppose that the event
was caused by the combination of synchronized venting or two independent
orifices. A small time delay between the initiation of venting from the
first and the second orifice, combined with perspective effects, can
reproduce both the highly collimated beam and the spiral structure at the
end of it. In this model, one orifice causes the collimated beam and the
second the spiral structure. Support for a dust model is given by the fact
that the velocity of expansion is very much lower than the gas velocity for
CO expulsion ([∼]30 m s-1 against [∼]1000 m s-1), although the true
velocity may be significantly higher if we are looking along the jet.
Given the observed timescale of jet events (approximately one per
month), it is statistically implausible that two independent venting
episodes would be triggered nearly simultaneously. The fact that a later
jet has produced a somewhat similar morphology with a position angle close
to 000° makes us reluctant to accept this model at present, despite its
obvious attractions. A further problem that has yet to be fully addressed
is whether the venting is a single instantaneous event (see below) or a
continuous emission over a number of days; significant difficulties with
the fit are found if a long duration of emission is assumed. A
long-duration event, though, is more in accord with the thermal triggering
mechanism and long rotation period that have been proposed to explain the
venting (Sekanina 1995d).
An alternative method (Shulman 1995, private communication) proposes
to explain the jet in terms of an invisible gas beam carrying visible dust
within it. The jet is seen as a two-dimensional projection of an Archimedes
spiral. This method does not require synchrone trajectories, thus removing
one potential difficulty, although it is similar in some respects to the
model proposed by Sekanina. An important difference is that this model
assumes a single emission event of very short duration, thus avoiding some
of the morphological difficulties. No specific triggering mechanism is
assumed, although thermal triggering is felt to be unlikely. The model is
proving to be promising in its results and, contrary to the synchrone
model, suggests that the different jets originate from different points on
the nucleus. However, it requires further development, given that some
aspects of the jets' development are still problematic at present,
particularly the derived ages of different parts of the jet.
We have been struck by the peculiar morphology of the August jet
event, some aspects of which appear more consistent with a plasma event
than with pure dust emission. The jet shows a very narrow, highly
collimated section that expands away from the nucleus. This shows a 90°
break at a projected distance initially of 23,000 km, at which point the
material directs itself very precisely in the antisolar direction. This
could be due to a chance alignment, and it is also consistent with a
plasma-jet model. The ejected material proceeds outward until it reaches
the contact surface and is open to the influence of the solar wind. At this
point, solar wind pickup occurs and the position angle is abruptly changed
as it sweeps round the contact surface until it reaches a position angle
corresponding to the antisolar direction. The fact that the end of the jet
was very closely aligned with the antisolar direction 2 favors a plasma
model.
Our data limit any possible position angle change in the jet to a
maximum of [∼]15°, which implies that, if the jet is caused by plasma,
it is located close to, but not at, the pole of the nucleus. This is
consistent with the slight jitter that is seen in the position angle
between the grouped integrations. This jitter is less easy to explain given
a dust-jet model.
We find that the point of inflection, where the jet suddenly comes
under the influence of the solar wind, is at a projected distance
[∼]23,000[–]39,000 km from the nucleus, according to the date of
observation. This gives us an estimate of the projected distance of the
contact surface, where a local equilibrium exists between the pressure of
the solar wind and the gas pressure within the inner coma. The angular
distance of the point of inflection from the nucleus is seen to increase
with time. This is not a perspective effect, since the geocentric distance
was increasing slowly during the observations, but rather reflects what
would be a genuine increase in the radius of the contact surface (Table 2).
This we can understand if there was a significant increase in gas
production corresponding to the jet event, and if the contact surface
expands until reaching a new pressure equilibrium.
Figure 2 shows the variation of the linear extent of the collimated
jet with time. Note that these are projected distances, and that the true
distances, and hence the derived velocity of expansion, may be much greater
if the viewing angle of the jet is not close to 90°. To make the plasma jet
model more plausible, we have to suppose that there is a significant
projection effect and that the length of the collimated jet is actually
significantly greater than 23,000 km; this would permit a significant
fraction of the molecules in the jet to become ionized, even if the density
of ions in the inner coma as a whole is rather low.
An obvious difficulty with this model is the lack of visible ions in
the spectrum. The most likely species to be detected at high heliocentric
distance, because of its abundance and very strong lines, is CO+.
Observations in the submillimetric range have shown significant neutral CO
emission, with a production rate when no jet was active of [∼]1 tonne
s-1 (Matthews, Jewitt, & Senay 1995; Rauer et al. 1995), but no reports
have been made of the presence of CO+ lines in the spectrum. Other species,
though, may exist that do not have easily detectable lines. IUE
observations have established an upper limit to H2O production, although
this corresponds to 3 tonnes s-1. Since H2O is a high-temperature volatile,
it is unlikely to be more active than CO anyway. An alternative
low-temperature volatile is NH3; the NH[$\mathstrut{^{+}_{2}}$] line is a
well-known line in cometary spectra but is very weak and difficult to
detect, except in very high S/N spectra.
Assuming that the jet is well described by a gaseous emission, which
is later photoionized, and that the emission is slow enough to permit the
coma to be in a quasi[–]steady state, the distance between the
nucleus and the point of inflection can, in theory, be used to make an
estimate of the total gas production rate. This assumes a model suggested
by Schmidt & Wegmann (1982). Various difficulties are found that obviate
the possibility of obtaining a firm numerical estimate, in particular, the
fact that only the projected distance of the point of inflection is known.
This very simple model would give a rather high total production rate
compared with the measured production rate of CO or the upper limit to H2O.
Since the CO production rate was measured with a quiescent nucleus, it is
not impossible that at the peak of outburst the production rate could be 2
orders of magnitude higher than this quiescent level ([∼]100 tonnes
s-1). The observation of large variations in the total brightness of the
comet and morphological changes reported by visual and CCD observers (e.g.,
formation of an intense starlike nucleus) lends support to the idea of a
highly variable production rate.
None of the three models that have been proposed are at this juncture
wholely satisfactory, and further work is needed on all of them. This means
that the plasma-jet model cannot be rejected simply because there is a
proved alternative explanation that renders it unnecessary.
FOOTNOTES
2 Something similar is observed with the September jet-event and
probably with the October event, suggesting that this is not simply
coincidence, given the rather different morphologies, position angles, and
evolution that have been seen.
§5. CONCLUSIONS
This paper presents a small subset of our data that covers 46 nights
of imaging to the last week of October. Work is progressing on detailed
modeling of the observations taken so far, including photometric
calibration and, where available, color information. A more detailed report
on our monitoring is being prepared (Kidger et al. 1996). We hope that
further analysis will allow us to differentiate more exactly between
models.
We find that the jet observed in comet Hale-Bopp (1995 O1) between
1995 August 25 and September 7 shows a highly characteristic morphology and
evolution. Some aspects of this morphology and evolution are challenging to
dust-ejection models and may be more consistent with a plasma model. No
single model, though, is totally satisfactory, and we hope that the
observations reported here will open a debate on the various possible
models and their limitations. We stress that the observed morphology,
distances, and velocities reported are projected values only and may bear
no relation to the true situation. Observations of the comet are
continuing, and a detailed examination of the different events observed to
date may shed more light on their causes and the validity of the different
models.
ACKNOWLEDGMENTS
The authors would like to thank the telescope operators at Teide
Observatory (Luis Chinarro, Angel Gómez, Luis Manadé, and Santiago López)
for their work in taking images of the comet during the extended monitoring
campaign, and Jesús Jiménez for making the telescope readily available to
us.
REFERENCES
* Hale, A., & Bopp, T. 1995, IAU Circ., No. 6187
* Jewitt, D. C., & Chen, J. 1995, IAU Circ., No. 6216 First citation in
article
* Kidger, M. R. 1995, Earth Moon Planets, in press First citation in
article
* Kidger, M. R., et al. 1996, in preparation First citation in article
* Marsden, B. G. 1995, IAU Circ., No. 6202 First citation in article
* Matthews, H. E., Jewitt, D., & Senay, M. C. 1995, IAU Circ., No. 6234
First citation in article
* Offut, W. 1995, IAU Circ., No. 6194 First citation in article
* Rauer, H., Despois, D., Moreno, R., & Paubert, G. 1995, IAU Circ., No.
6236 First citation in article
* Schmidt, H. U., & Wegmann, R. 1982, in Comets, ed. L. L. Wilkening
(Tucson: Univ. Arizona Press), 538 First citation in article
* Sekanina, Z. 1995a, IAU Circ., No. 6194 First citation in article
* [—][—][—]. 1995b, IAU Circ., No. 6223 First citation
in article
* [—][—][—]. 1995c, IAU Circ., No. 6240 First citation
in article
* [—][—][—]. 1995d, IAU Circ., No. 6248 First citation
in article
* West, R. 1995, IAU Circ., No. 6226 First citation in article
FIGURES
[Image] Full image (117kb) [Image] Full image (140kb) [Image] Full image
(140kb) [Image] Full image (138kb) [Image] Full image (130kb) | Discussion
in text
Fig. 1.[—]Processed images of the near-nucleus region of comet
Hale-Bopp (1995 O1) from (a) August 15, (b) August 25, (c) August 27, (d)
August 28, and (e) August 31. Contours of the coma brightness have been
drawn only at distances well beyond the jet, to show that the outer coma
was very nearly circular at this time, despite the near-nucleus activity.
Contours are drawn at intervals from 1 [σ] to 5 [σ] of the sky
brightness. The direction of the projected cometary velocity vector (
[$\mathstrut{{\bmi v}}$]) and the antisolar direction (
[$\mathstrut{{\bmi r}}$]) are marked, along with the scale and orientation
of the figures.
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[Image] Full image (5kb) | Discussion in text
Fig. 2.[—]Evolution of the length of the jet from the nucleus to
the point of inflection over the period covered by these observations. A
steady increase in length can be seen.
TABLES
TABLE 1
Observing Log for the Observations of the Jet
Total
Number of Exposure
UT Date Band Images UT Range (s) Notes
Aug 15... R 6 22:33[–]23:12 2400
Aug 25... R 21 21:19[–]23:47 7400
Aug 27... R 6 20:35[–]22:33 1620 Cirrus
Aug 28... B 23 21:06[–]23:21 6800 Cirrus
Aug 31... R 15 20:12[–]21:45 4500 Cirrus
Sep 4... R 42 20:51[–]23:00 5040
Sep 5... R 23 20:35[–]22:49 6900 Cirrus
Sep 6... R 24 20:24[–]22:50 7200
Sep 7... R 14 21:23[–]22:42 7200
Sep 8... R 23 20:31[–]22:44 6900
Image of typeset table (28kb) | Discussion in text
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TABLE 2
Details of the Observations of the Jet a
Linear Extent
Date UT Time Angular Extent (km)
Aug 25... 21:19 5[&farcs;]4 24,500
Aug 25... 22:13 5[&farcs;]0 22,500
Aug 25... 23:11 5[&farcs;]4 24,500
Aug 27... 20:34 5[&farcs;]8 26,500
Aug 28... 20:56 7[&farcs;]3 33,400
Aug 28... 21:48 7[&farcs;]1 32,400
Aug 28... 22:44 7[&farcs;]3 33,400
Aug 31... 21:01 8[&farcs;]6 39,300
Sep 4... 21:56 11[&farcs;]2 51,400
a Note.[—]The angular and linear extent refer to the distance
between the nucleus and the point of inflection where the jet is swept back
by the solar wind.
Image of typeset table (27kb) | Discussion in text
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