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DOI: 10.1051/0004-6361:20053054
Observations in the Saturn system during approach and orbital insertion, with Cassini's visual and infrared mapping spectrometer (VIMS)
R. H. Brown1, K. H. Baines2, G. Bellucci3, B. J. Buratti2, F. Capaccioni4, P. Cerroni4, R. N. Clark5, A. Coradini4, D. P. Cruikshank6, P. Drossart7, V. Formisano3, R. Jaumann8, Y. Langevin9, D. L. Matson4, T. B. McCord10, V. Mennella11, R. M. Nelson4, P. D. Nicholson12, B. Sicardy7, C. Sotin13, N. Baugh1, C. A. Griffith1, G. B. Hansen10, C. A. Hibbitts10, T. W. Momary2 and M. R. Showalter61 Department of Planetary Sciences, and Lunar and Planetary Laboratory, University of Arizona, 1629 E. University Boulevard, Tucson, AZ 85721, USA
e-mail: rhb@lpl.arizona.edu
2 Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Boulevard, Pasadena, CA 91109, USA
3 Consiglio Nazionale delle Ricerche, Isituto di Fisica dello Spazio Interplanetario, Via Fosso del Cavaliere, Tor Vergata, 00133 Roma, Italy
4 Consiglio Nazionale delle Ricerche, Isituto di Astrofisica Spaziale, via Fosso del Cavaliere, Tor Vergata, 00133 Roma, Italy
5 Mail Stop 964, US Geological Survey, Box 25046, Denver Federal Center, Denver, CO 80225, USA
6 Mail Stop 245-6, NASA Ames Research Center, Moffett Field, California 94035, USA
7 Observatoire de Paris, Meudon, Department de Recherche Spatial, 5 Place Jules Janssen, 92195 Meudon Cedex, France
8 Institute for Planetary Exploration, Deutsches Zentrum for Luft und Raumfahrt, Rudower Chausee 5, 12489 Berlin, Germany
9 Institute d'Astrophysique Spatiale, Université de Paris, Bâtiment 121, 91405 Orsay Cedex, France
10 Department of Earth and Space Sciences, Johnson Annex A, Box 351310, University of Washington, Seattle WA 98195, USA
11 Istituto Nazionale di Astrofisica, Observatorio Astronomico di Capodimonte, via Moiariello 16, 80131 Napoli, Italy
12 Department of Astronomy, Cornell University, Ithaca, NY 14853, USA
13 Laboratoire de Planetologie et Geodynamique, UMR - CNRS 6112, Faculty des Sciences, BP 92208, 2 rue de la Housseni
(Received 13 March 2005 / Accepted 8 August 2005 )
Abstract
The Visual and Infrared Mapping Spectrometer observed Phoebe,
Iapetus, Titan and Saturn's rings during Cassini's approach and
orbital insertion. Phoebe's surface contains water ice, CO2,
and ferrous iron. Iapetus contains CO2 and organic materials.
Titan's atmosphere shows methane fluorescence, and night-side
atmospheric emission that may be CO2 and CH3D. As
determined from cloud motions, the winds at altitude 25-30 km in
the south polar region of Titan appear to be moving in a prograde
direction at velocity
1 m s-1. Circular albedo
features on Titan's surface, seen at 2.02
m, may be
palimpsests remaining from the rheological adjustment of ancient
impact craters. As such, their long-term persistence is of special
interest in view of the expected precipitation of liquids and
solids from the atmosphere. Saturn's rings have changed little in
their radial structure since the Voyager flybys in the early
1980s. Spectral absorption bands tentatively attributed to
Fe2+ suggest that iron-bearing silicates are a source of
contamination of the C ring and the Cassini Division.
Key words: infrared: solar system -- planets and satellites: general
© ESO 2006
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