Considering Papers I and II together with this work, the complete range of
nuclear radii estimates for the unresolved comets is
0.92 km
km, while the range of 3
upper limits for
the active and undetected comets is 0.5 km
km. An
albedo of 0.04 was assumed throughout, with the exception of comets for
which the albedo has been previously measured. Appendix A
brings together each nuclear radius result from Papers I, II, and III into one
table. This table also states whether the comet was active, unresolved, or
undetected, and whether the comet was on its inbound or outbound leg of its orbit.
In deriving the absolute magnitude of the active comets the
following expression is used:
For active comets, the constant n is generally assumed to have a value of 4. Essentially, this term accounts for variations of the total scattering cross-section with heliocentric distance, which is caused by changes in the dust production levels with heliocentric distance. For the unresolved and undetected comets, we assume n = 2, as expected for inert bodies.
Figure 5a plots the cumulative
number of comets with magnitudes brighter than
R(1,1,0) versus
R(1,1,0)for the active and unresolved
comets combined, as-well as for the unresolved comets only. Considering the curve
where the data for the active comets and unresolved comets are combined, it is
clear that the slope of this curve is best represented by a broken power law for
absolute magnitudes brighter than 15.5. Therefore the Cumulative Luminosity Function
(CLF) of the absolute magnitudes of our entire sample of 33 detected comets can
be described by:
![]() |
Figure 5:
(a) The number of comets <
R(1,1,0) versus
absolute R band magnitude
R(1,1,0) for the active and unresolved comets
combined (triangles), as-well as the number of comets <
R(1,1,0)
versus
R(1,1,0) for the unresolved comets only (circles).
(b) Same as (a), but with a logarithmic y axis. A
slope of
![]() |
More important is the CLF of the unresolved comets. Fernández et al.
(1999) have addressed this issue, but they used data from many
different sources, with some dating back as far as 1950. The vast
majority of their `best estimates' for the nuclear magnitudes derive from
inconsistent reduction methods and a significant portion rely upon
less-than-optimal coma subtraction techniques. In addition, one cannot be sure
if the derived magnitudes have been transformed onto a common photometric
system. This makes inter-comparison of data between individual comets extremely
difficult. Nevertheless, they have used these data in an attempt to constrain
the CLF of the Jupiter-family comets. They plot Log
versus absolute visual nuclear magnitude
V(1,1,0) for comets with
perihelion distances <2 AU. Using these data, Fernández et al. find that
the CLF follows a linear relation within the small magnitude range of
15.25 < V(1,1,0) < 16, with a gradient of 0.54.
As shown in Fig. 5b, a least-squares fit to our
data for unresolved nuclei implies a slope for the CLF of
,
within the large absolute magnitude range of
14.5 < R(1,1,0) < 16.5.
This gradient is significantly different from Fernández et al.
(1999), but as our data is derived using homogeneous
reduction methods and is entirely CCD based, we believe that this slope
represents the most realistic estimate of the size distribution of
Jupiter-family comets to date.
Now that we have an estimate of the CLF slope for the Jupiter-family comets,
we can derive the size and mass distributions of the Jupiter-family population.
The CLF for Jupiter-family comets is of the form:
It is unlikely that the size distribution of the ejected TNOs
would be preserved upon entering the inner solar system, due to the various
processes acting upon the nucleus that would inevitably change their physical
characteristics. Such processes include tidal disruption by the giant planets
(Sekanina 1997), fragmentation due to intense solar heating
(Delahodde et al. 2000; Filippenko & Chornock 2000),
and nuclear sublimation. Unfortunately, such processes would increase the slope
of the CLF, and not decrease it as required by our data. Therefore how can we
account for a CLF slope for the Jupiter-family comets of
presented here? One explanation for this effect could be the observational
bias towards the discovery of larger Jupiter-family comets, or at least those
with a significant active surface area. If our measured value is truly
intrinsic to the population however, then perhaps Solar heating leads to
complete disintegration of small cometary nuclei or at least their rapid diminution
to below observational detection limits, which would result in a further
decrease in the slope of the CLF.
If indeed there is a progressive decrease in the slope of the CLF as comets
evolve from the Edgeworth-Kuiper belt to the realm of the Jupiter-family comets,
then a precise determination of the CLF of the Centaur population may prove
valuable. Unfortunately, the discovery rate of Centaurs is relatively slow at
present, but wide field CCD surveys are being conducted, with preliminary values
for the slope of the Centaur CLF of
0.6 (Sheppard et al. 2000) and
0.54 (Larsen et al. 2001).
Finally, it is interesting to note that our derived value for
of
is similar to that for main-belt asteroids according to
Jedicke & Metcalf 1998, who found
but with large
variations. Also, recent estimates for the CLF slope parameter of Near Earth
Objects are 0.35 (Rabinowitz 2000; Bottke et al. 2001),
and 0.39 (Stuart 2001). Hence these two collisionally dominated populations
display size distributions significantly different from the theoretically
expected value of
(Dohnanyi 1969; Williams & Wetherill
1994).
Considering the activity levels of the Jupiter-family population as a whole,
this survey clearly illustrates the diverse levels of activity present beyond
3 AU from the Sun, and that for several comets the levels of activity are
substantial. From Papers I, II, and III, the measured
values for the
active comets range from
cm to
cm.
Correlations between the activity levels of the comets in our sample
and their various orbital parameters were investigated. The only correlation we
found for our sample was between intrinsic brightness and
perihelion distance. Figure 6 plots the absolute R band
magnitude
R(1,1,0) versus perihelion distance for every comet observed
throughout the survey, and
also includes most of the 3
upper limits obtained for the
undetected comets. For the active comets in Fig. 6,
the plotted magnitudes are the total magnitudes, i.e. nucleus plus coma.
Several of the comets in this sample were targeted on separate observing runs,
therefore upper limits for undetected comets that were previously or
subsequently detected, have been discarded. Also, for comets that were
observed to be stellar in appearance on several occasions, the mean absolute
magnitude is taken.
![]() |
Figure 6:
This figure is a plot of the absolute R band
magnitude
R(1,1,0) versus perihelion distance for the comets observed in this
survey, and also includes most of the 3![]() |
In Fig. 6, the active comets are represented by filled
circles, whereas the unresolved and undetected comets are represented by open
circles and stars respectively.
For the active comets only, there appears to be a
distinct correlation between absolute R band magnitude and the comets
perihelion distance, i.e. the intrinsic brightness increases with
perihelion distance. Performing a least squares fit to these data points yields
a slope of
.
Accurate knowledge of the parameter n for each
individual comet may reduce the scatter in the data points and hence the
associated uncertainty, however it is believed that the upward trend seen in
Fig. 6 for the active comets is a genuine feature.
This effect can be interpreted either as a discovery bias towards brighter comets, or in terms of mantle formation, specifically the "Rubble'' mantle hypothesis. Recent arrivals to the inner Solar system should have relatively large fractional sublimating areas. As these new Jupiter-family comets are perturbed inwards, prolonged sublimation produces a rubble mantle which reduces the amount of free sublimating area and hence the brightness of the cometary coma at all heliocentric distances. The rubble mantle would continue to spread across the nuclear surface as the comet spends a larger fraction of its orbital period at progressively smaller heliocentric distances. This would imply the existence of a correlation between the amount of active area and/or composition, with perihelion distance. Such a correlation between the amount of active area and perihelion distance has been seen previously by (A'Hearn et al. 1995), albeit extremely weakly.
![]() |
Figure 7: This figure plots the "best estimates'' for the visual nuclear magnitude V(1,1,0) versus perihelion distance. These data are from Fernández et al. (1999). |
A similar correlation between intrinsic brightness and perihelion distance
is not seen for the unresolved and undetected comets, despite a
wide range of perihelion distances. This finding is compared with the data
presented in Fernández et al. (1999).
Figure 7 plots their "best estimates'' for the
visual nuclear magnitudes versus perihelion distance. An apparent upward trend
is seen and if one performs a least squares fit to the data points, then a linear
relation with gradient
describes the data well.
This value is remarkably similar to the slope seen for the active comets of Fig. 6. Hence, the illusion of an upward trend in
Fig. 7 may be created if the comets
with large perihelion distances are actually outgassing.
Indeed, if one removes comets with perihelion distances beyond 3 AU
(which is only 16% of the comets in their sample), then one is left with a
random scatter of data points, spread over a magnitude range similar to that
of the unresolved and undetected comets of Fig. 6.
Therefore, based on this argument and the data presented in
Fig. 6, we conclude that there is, as of yet,
no correlation between absolute nuclear magnitudes and perihelion
distance.
Copyright ESO 2003