Search Publications

Titan solar occultation observed by Cassini/VIMS: Gas absorption and constraints on aerosol composition
DOI: 10.1016/j.icarus.2008.12.024 Bibcode: 2009Icar..201..198B

Baines, K. H.; Nicholson, P. D.; Drossart, P. +5 more

A solar occultation by Titan's atmosphere has been observed through the solar port of the Cassini/VIMS instrument on January 15th, 2006. Transmission spectra acquired during solar egress probe the atmosphere in the altitude range 70 to 900 km at the latitude of 71° S. Several molecular absorption bands of CH 4 and CO are visible in thes…

2009 Icarus
Cassini 71
Lineated valley fill (LVF) and lobate debris aprons (LDA) in the Deuteronilus Mensae northern dichotomy boundary region, Mars: Constraints on the extent, age and episodicity of Amazonian glacial events
DOI: 10.1016/j.icarus.2009.02.017 Bibcode: 2009Icar..202...22M

Head, James W.; Marchant, David R.; Morgan, Gareth A.

In order to assess the nature, degradational processes and history of the dichotomy boundary on Mars, we conducted a detailed morphological analysis of a 70,000 km2 region of its northern portion (north-central Deuteronilus Mensae, south of Lyot, in the vicinity of Sinton Crater). This region is characterized by the distinctive sinuous …

2009 Icarus
MEx 70
3D triangulation of a Sun-grazing comet
DOI: 10.1016/j.icarus.2008.12.011 Bibcode: 2009Icar..200..351T

Thompson, W. T.

The bright Kreutz Comet C/2007 L3 (SOHO) entered the fields of view of the twin Solar Terrestrial Relations Observatory (STEREO) COR1 telescopes on 7-8 June 2007. The 12° separation between the two spacecraft at the time afforded the opportunity to derive the position of the comet's tail in three-dimensional space using direct triangulation. The t…

2009 Icarus
SOHO 67
Shoreline features of Titan's Ontario Lacus from Cassini/VIMS observations
DOI: 10.1016/j.icarus.2008.12.028 Bibcode: 2009Icar..201..217B

Sotin, Christophe; Barnes, Jason W.; Soderblom, Jason M. +12 more

We analyze observations of Titan's south polar lake Ontario Lacus obtained by Cassini's Visual and Infrared Mapping Spectrometer during the 38th flyby of Titan (T38; 2007 December 5). These near-closest-approach observations have the highest signal-to-noise, the finest spatial resolution, and the least atmospheric influence of any near-infrared la…

2009 Icarus
Cassini 65
Crater modification and geologic activity in Enceladus' heavily cratered plains: Evidence from the impact crater distribution
DOI: 10.1016/j.icarus.2009.03.034 Bibcode: 2009Icar..202..656K

Schenk, Paul; Kirchoff, Michelle R.

Although we can observe current activity on Saturn's satellite Enceladus with Cassini, insight into past activity is best achieved (for now) through studying the impact crater distributions. Furthermore, approximation of terrain ages can only be attained through calculations using crater densities and estimations of impact rates in the saturnian s…

2009 Icarus
Cassini 64
The detached haze layer in Titan's mesosphere
DOI: 10.1016/j.icarus.2009.01.004 Bibcode: 2009Icar..201..626L

Lavvas, Panayotis; Yelle, Roger V.; Vuitton, Véronique

By comparing observations from the Cassini imaging system, UV spectrometer, and Huygens atmospheric structure instrument, we determine an apparent radius of ∼40 nm, an imaginary index <0.3 at 187.5 nm and a number density of ∼30 particles cm -3 for the detached haze layer at 520 km in Titan's mesosphere. We point out that the detache…

2009 Icarus
Huygens 61
Endogenic heat from Enceladus' south polar fractures: New observations, and models of conductive surface heating
DOI: 10.1016/j.icarus.2008.07.016 Bibcode: 2009Icar..199..189A

Spencer, John R.; Abramov, Oleg

Linear features dubbed "tiger stripes" in the south polar region of Enceladus have anomalously high heat fluxes and are the apparent source of the observed plume. Several explanations for the observed activity have been proposed, including venting from a subsurface reservoir of liquid water, sublimation of surface ice, dissociation of clathrates, …

2009 Icarus
Cassini 59
Io's dayside SO 2 atmosphere
DOI: 10.1016/j.icarus.2009.01.029 Bibcode: 2009Icar..201..570F

Feldman, Paul D.; Feaga, Lori M.; McGrath, Melissa

An extensive set of HI Lyman- α images obtained with the Hubble Space Telescope (HST) Space Telescope Imaging Spectrograph (STIS) from 1997-2001 has been analyzed to provide information about the spatial and temporal character of Io's SO 2 atmosphere. An atmospheric distribution map derived from the observations reveals that the sunlit …

2009 Icarus
eHST 59
Possible pingo fields in the Utopia basin, Mars: Geological and climatical implications
DOI: 10.1016/j.icarus.2008.09.007 Bibcode: 2009Icar..199...49D

de Pablo, Miguel Ángel; Komatsu, Goro

The presence of pingos on Mars has been hypothesized since the period of the Viking mission. In fact, a diverse range of pingo-like features has been found at various martian sites including Elysium, Chryse and Utopia Planitiae in the northern lowlands. Due to the morphology and the geological setting, some of those features were interpreted in di…

2009 Icarus
MEx 59
Quantitative compositional analysis of martian mafic regions using the MEx/OMEGA reflectance data 1. Methodology, uncertainties and examples of application
DOI: 10.1016/j.icarus.2008.12.025 Bibcode: 2009Icar..201...69P

Mangold, N.; Bibring, J. -P.; Gondet, B. +7 more

The Mars Express Observatoire pour la Minéralogie, l'Eau, les Glaces et l'Activité (OMEGA) collected an unprecedented visible and near-infrared hyperspectral dataset covering the low albedo regions of Mars. We investigate the ability to infer modal abundance of surfaces of these regions from a radiative transfer model developed by Shkuratov et al.…

2009 Icarus
MEx 59