http://www.cnr.it/ontology/cnr/individuo/prodotto/ID45232
Characterization of Titan's Ontario Lacus region from Cassini/VIMS observations (Articolo in rivista)
- Type
- Label
- Characterization of Titan's Ontario Lacus region from Cassini/VIMS observations (Articolo in rivista) (literal)
- Anno
- 2010-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1016/j.icarus.2010.07.023 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- M. L. Moriconi (a); J. I. Lunine (b)(e); A. Adriani (b); E. D'Aversa (b); A.Negrão (b)(c); G. Filacchione (d); A. Coradini (b) (literal)
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- Accepted for publication (literal)
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- ISI Web of Science (WOS) (literal)
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- (a) Institute of Atmospheric Science and Climate-CNR, Via Fosso del Cavaliere 100, I-00133 Rome, Italy
(b) IFSI-INAF, Via Fosso del Cavaliere 100, I-00133 Rome, Italy
(c) Escola Superior de Tecnologia e Gestão de Leiria, Campus 2, Morro do Lena-Alto do Vieiro, P-2411 Leiria, Portugal
(d) IASF-INAF, Via Fosso del Cavaliere 100, I-00133 Rome, Italy
(e) Department of Physics, University of Rome Tor Vergata, Via della Ricerca Scientifica 1, 00133 Roma, Italy (literal)
- Titolo
- Characterization of Titan's Ontario Lacus region from Cassini/VIMS observations (literal)
- Abstract
- Liquid hydrocarbons were long predicted on Titan's surface before the RADAR instrument onboard Cassini
detected lakes poleward of 70?N in July 2006. Before that the Cassini Imaging Science Subsystem (ISS)
observed a lake-like feature in the South Pole, named Ontario Lacus, in July 2004. Here we analyze one
observation of Ontario Lacus taken by the Visual and Infrared Mapping Spectrometer (VIMS) on 2007
December 5, during the T 38 flyby. This is the best spatially resolved image of a Titan lake to date by
an imaging spectrometer, and has been previously reported in Brown et al. (Brown, R.H., Soderblom,
L.A., Soderblom, J.M., Clark, R.N., Jaumann, R., Barnes, J.W., Sotin, C., Buratti, B., Baines, K.H., Nicholson,
P.D. [2008]. Nature 454, 607-610) and in Barnes et al. (Barnes, J.W. et al. [2009]. Icarus 201, 217-225).
The observing geometry and our data processing will be explained, followed by a discussion of the main
characteristics of the image. The analyzed image covers a small portion of Ontario Lacus and shows what
appears from RADAR data to be a region of modest slope (''ramp\") adjacent to the dark lake itself. Our
analysis of 5.0 lm spectral data suggests that the previously reported absorption feature of ethane seen
at shorter wavelengths may be produced by damp sediments adjacent to the main liquid basin. The latter
appears to be absorbing all of the photons incident upon it in the 5 lm spectral region and shows no discernible
absorption features. A characterization of the basin composition and morphology is developed
with the help of ISS and RADAR observations. The simplest model consistent with the data is an optically
deep lake surrounded by a region in which ethane, propane, possibly methane, and other, less volatile
hydrocarbons and nitriles are present mixed into spectroscopically neutral sediments. The dominance
of relatively low vapor pressure organics outside the lake itself suggests a retreat of Ontario Lacus associated
with evaporation on seasonal or longer timescales, consistent with analysis of RADAR and ISS
images. (literal)
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