Bibcode
Ortiz, J. L.; Duffard, R.; Pinilla-Alonso, N.; Alvarez-Candal, A.; Santos-Sanz, P.; Morales, N.; Fernández-Valenzuela, E.; Licandro, J.; Campo Bagatin, A.; Thirouin, A.
Referencia bibliográfica
Astronomy and Astrophysics, Volume 576, id.A18, 12 pp.
Fecha de publicación:
4
2015
Revista
Número de citas
97
Número de citas referidas
87
Descripción
We propose that several short-duration events observed in past stellar
occultations by Chiron were produced by ring material. Some similarities
between these events and the characteristics of Chariklo's rings could
indicate common mechanisms around centaurs. From a reanalysis of the
stellar occultation data in the literature, we determined two possible
orientations of the pole of Chiron's rings, with ecliptic coordinates
λ = (352 ± 10)°, β = (37 ± 10)° or
λ = (144 ± 10)°, β = (24 ± 10)°. The
mean radius of the rings is (324 ± 10) km. One can use the
rotational lightcurve amplitude of Chiron at different epochs to
distinguish between the two solutions for the pole. Both solutions imply
a lower lightcurve amplitude in 2013 than in 1988, when the rotational
lightcurve was first determined. We derived Chiron's rotational
lightcurve in 2013 from observations at the 1.23 m CAHA telescope, and
indeed its amplitude was smaller than in 1988. We also present a
rotational lightcurve in 2000 from images taken at the CASLEO 2.15 m
telescope that is consistent with our predictions. Out of the two poles,
the λ = (144 ± 10)°, β = (24 ± 10)°
solution provides a better match to a compilation of rotational
lightcurve amplitudes from the literature and those presented here. We
also show that using this preferred pole orientation, Chiron's long-term
brightness variations are compatible with a simple model that
incorporates the changing brightness of the rings while the tilt angle
with respect to the Earth is changing with time. Also, the variability
of the water ice band in Chiron's spectra as seen in the literature can
be explained to a large degree by an icy ring system whose tilt angle
changes with time and whose composition includes water ice, analogously
to the case of Chariklo. We present several possible formation scenarios
for the rings from qualitative points of view and speculate on why rings
might be common in centaurs. We also speculate on whether the known
bimodal color distribution of the centaurs could be due to centaurs with
rings and centaurs without rings.
Table 1 is only available at the CDS via anonymous ftp to http://cdsarc.u-strasbg.fr
(ftp://130.79.128.5) or via http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/576/A18
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