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A&A 445, 1151-1157 (2006)
DOI: 10.1051/0004-6361:20053833
Pre-impact monitoring of Comet 9P/Tempel 1, the Deep Impact target
L. M. Lara1, H. Boehnhardt2, R. Gredel3, P. J. Gutiérrez1, J. L. Ortiz1, R. Rodrigo1 and M. J. Vidal-Nuñez11 Instituto de Astrofísica de Andalucía, CSIC, PO Box 3004, 18080 Granada, Spain
e-mail: lara@iaa.es
2 Max-Planck Institut für Sonnensystemforschung, Max-Planck-Str. 2 37191 Katlenburg-Lindau, Germany
e-mail: boehnhardt@mps.mpg.de
3 Max-Planck Institut für Astronomie, Königstuhl 17, 69117 Heidelberg, Germany
e-mail: gredel@caha.es
(Received 15 July 2005 / Accepted 14 September 2005 )
Abstract
Comet 9P/Tempel 1, the target of the Deep Impact
Mission, has been monitored for 6 months aiming at its
characterization before the impact experiment. During this period
of time, the coma has gone through a slow morphological evolution from
a wide structure in the south-western quadrant in mid-February to a
porcupine pattern in mid-April and up to seven features identified
in June. In addition to this evolution, an arclet in the western
coma hemisphere was detected on June 14, related to an outburst
event. Interpretation of these features and their evolution seems
to indicate the presence of at least 3 or 4 very active regions on
the nucleus, consistent with the rotation axis being oriented close
to previous solutions found by Belton et al. (2005), or
close to the angular momentum vector of the orbital motion of the
comet. The value of
varies with heliocentric distance
as
; slightly enhanced
(above the
curve) was observed from mid-February until the end of March, when
fan-shaped structures appeared in the coma for the first
time. Somewhere between mid-April to mid-May (i.e. 80 to 60 days
before perihelion), the comet peaked in activity. In terms of gas
production rates, CN, C2 and C3 have been obtained at
, 1.60 and 1.51 AU, being slightly below those derived
from previous passages. Abundance ratios of these species indicate
that comet 9P/Tempel 1 is classified as typical in terms of C2
abundance. The surface brightness profiles of the continuum, either
azimuthally averaged profiles from the broadband images or in
north-south direction from the long-slit spectra can be well fit
with
in
representation. Steeper slopes are obtained at larger
which
might be related to variable dust size distribution with distance
from the nucleus due to the radiation pressure dynamics and/or
physical processing of the dust grains (sublimation,
fragmentation). Normalized color of the dust inside the coma in the
north-south direction is measured to be
.
Key words: comets: individual: 9P/Tempel 1
© ESO 2006
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