The nongravitational equations of the comet motion have been integrated numerically by the recurrent power series method, taking into account all the planetary perturbations (Sitarski 1979, 1984). Satisfactory solution for each of the six comets were found.
Numerical values of the nongravitational parameters as well as values
of the osculating orbital elements are given in Table 4. Solutions with the
positive values of
and oblateness s for comets
31P/Schwassmann-Wachmann 2 and 21P/Giacobini-Zinner (Table 4b) represent the
cometary model with the oblate spheroidal nucleus; the negative values of
and s obtained for comets 43P/Wolf-Harrington, 37P/Forbes
16P/Brooks 2 and 32P/Comas Solá (Table 4a) represent the prolate spheroid
(the nucleus rotates around its longer axis). According to our solution the
nucleus of 21P/Giacobini-Zinner with oblateness along the spin-axis of about
0.29 (equatorial to polar radius of 1.41) is the most oblate among all
six investigated comets and nucleus of 32P/Comas Solá with the ratio
of equatorial to polar radius of 0.78 being the most prolate one.
The motion of the nucleus rotation axis represented by
angles I and
and the qualitative variations of the
nongravitational force components
F1, F2, F3 acting on the
comet during its successive returns to the Sun are presented in
Figs. 4a-f. According to our models six comets precess in
different manner and at different rates; among them the precession
of 21P/Giacobini-Zinner is the most rapid one. One can see that
changes of F1, F2 and F3 for all comets studied are
significantly different. For comet Wolf-Harrington we notice a
spectacular increase of nongravitational force after reducing the
perihelion distance from 2.42 AU to 1.45 AU due to a close
approach to Jupiter in 1936. In the Schwassmann-Wachmann 2 case
two large changes of nongravitational force are visible; both due
to a close encounter with Jupiter (March 1926 within 0.179 AU and
March 1997 within 0.246 AU): the first - before comet discovery,
the second - after the last detection of the comet.
The present precession models impose some constraints on physical
properties of the nuclei of the comets. Using solutions shown in Tables 4a-b it
is possible to calculate values of Sekanina's (1984) torque factor
.
Then we are able to calculate the value of
ratio from the formula:
,
where the equatorial radius,
,
is related to the
oblateness and the polar radius,
:
.
Our
models give:
These relationships lie within the region occupied by
comets with well-determined sizes and rotation periods (see
Fig. 5). In Fig. 5 are also shown relationships between
effective radii and rotation periods resulting from other
investigations undertaken by Sitarski and collaborators for some
short-period comets.
Copyright ESO 2001