Search Publications

Near-infrared spectra of ferrous mineral mixtures and methods for their identification in planetary surface spectra
DOI: 10.1016/j.icarus.2014.02.031 Bibcode: 2014Icar..234..132H

Bell, James F.; Cloutis, Edward A.; Mann, Paul +1 more

Iron-bearing minerals are a major component of planetary surfaces, and many can be identified by their characteristic absorption bands in the near-infrared (NIR). Here we present laboratory NIR spectra of a wide range of common Fe-bearing minerals (e.g., olivines, pyroxenes), glasses, and mineral/glass mixtures. We then use this suite of spectra t…

2014 Icarus
Chandrayaan-1 MEx 143
Saturn ring seismology: Evidence for stable stratification in the deep interior of Saturn
DOI: 10.1016/j.icarus.2014.08.006 Bibcode: 2014Icar..242..283F

Fuller, Jim

Seismology allows for direct observational constraints on the interior structures of stars and planets. Recent observations of Saturn's ring system have revealed the presence of density waves within the rings excited by oscillation modes within Saturn, allowing for precise measurements of a limited set of the planet's mode frequencies. We construc…

2014 Icarus
Cassini 92
Chemical composition of Titan’s atmosphere and ionosphere: Observations and the photochemical model
DOI: 10.1016/j.icarus.2014.03.041 Bibcode: 2014Icar..236...83K

Krasnopolsky, Vladimir A.

Basic observational data on hydrocarbons, nitriles, and ions on Titan are compared with predictions of the photochemical model. Uncertainties of the observed abundances and differences between the data from different instruments and observing teams are comparable with the differences between the observations and the model results. Main reactions o…

2014 Icarus
Cassini 91
Shape, topography, gravity anomalies and tidal deformation of Titan
DOI: 10.1016/j.icarus.2014.03.018 Bibcode: 2014Icar..236..169M

Lunine, Jonathan I.; Hayes, Alex; Zebker, Howard +5 more

Gravity measurements and elevation data from the Cassini mission have been used to create shape, global topography and gravity anomaly models of Titan that enable an improved understanding of its outer ice I shell structure. We provide constraints on the averaged ice shell thickness and its long-wavelength lateral variations, as well as the densit…

2014 Icarus
Cassini 83
Coupling of oxygen, nitrogen, and hydrocarbon species in the photochemistry of Titan's atmosphere
DOI: 10.1016/j.icarus.2013.10.015 Bibcode: 2014Icar..228..324D

Dobrijevic, M.; Loison, J. C.; Hickson, K. M. +1 more

Analysis of recent detections of water by Herschel/HIFI-PACS and Cassini/CIRS suggest for a steep gradient of the water profile in the lower stratosphere of Titan's atmosphere (Cottini, V., Nixon, C.A., Jennings, D.E., Anderson, C.M., Gorius, N., Bjoraker, G.L., Coustenis, A., Teanby, N.A., Achterberg, R.K., Béezard, B., de Kok, R., Lellouch, E., …

2014 Icarus
Cassini 76
Titan’s internal structure inferred from its gravity field, shape, and rotation state
DOI: 10.1016/j.icarus.2014.04.007 Bibcode: 2014Icar..237...29B

Tobie, Gabriel; Lefèvre, Axel; Baland, Rose-Marie +1 more

Several quantities measured by the Cassini-Huygens mission provide insight into the interior of Titan: the second-degree gravity field coefficients, the shape, the tidal Love number, the electric field, and the orientation of its rotation axis. The measured obliquity and tides, as well as the electric field, are evidence for the presence of an int…

2014 Icarus
Cassini 70
Mud volcanism and morphology of impact craters in Utopia Planitia on Mars: Evidence for the ancient ocean
DOI: 10.1016/j.icarus.2013.09.018 Bibcode: 2014Icar..228..121I

Hiesinger, H.; Erkeling, G.; Reiss, D. +1 more

Results of our detailed geological mapping and interpretation of the nature and relative and absolute model ages of units and structures in the SW portion of Utopia Planitia (20-45°N, 100-120°E) suggest the following. (1) The size-frequency distribution (SFD) of craters that both are buried by materials of the Vastitas Borealis units (VB) and supe…

2014 Icarus
MEx 68
Global mapping and characterization of Titan's dune fields with Cassini: Correlation between RADAR and VIMS observations
DOI: 10.1016/j.icarus.2013.11.017 Bibcode: 2014Icar..230..168R

Le Mouélic, S.; Cornet, T.; Rodriguez, S. +18 more

Vast fields of linear dunes have been observed in the equatorial regions of Titan, Saturn's largest moon. As the Cassini mission, in orbit around Saturn since July 2004 and extended until May 2017, carries on, the high-resolution coverage of Titan's surface increases, revealing new dune fields and allowing refinements in the examination of their p…

2014 Icarus
Cassini 65
Evidence for a bimodal size distribution for the suspended aerosol particles on Mars
DOI: 10.1016/j.icarus.2013.12.015 Bibcode: 2014Icar..231..239F

Maltagliati, L.; Montmessin, F.; Bertaux, J. -L. +4 more

First simultaneous analysis of the ultraviolet (UV) and infrared (IR) atmospheric extinctions from SPICAM/Mars Express solar occultations in the beginning of the Northern summer (Ls = 56-97°) is presented. The two SPICAM channels allow sounding of the martian atmosphere in the spectral range from 0.118 to 1.7 µm at the altitudes f…

2014 Icarus
MEx 64
Evidence of Titan's climate history from evaporite distribution
DOI: 10.1016/j.icarus.2014.08.022 Bibcode: 2014Icar..243..191M

Sotin, Christophe; MacKenzie, Shannon M.; Barnes, Jason W. +8 more

Water-ice-poor, 5-µm-bright material on Saturn's moon Titan has previously been geomorphologically identified as evaporitic. Here we present a global distribution of the occurrences of the 5-µm-bright spectral unit, identified with Cassini's Visual Infrared Mapping Spectrometer (VIMS) and examined with RADAR when possible. We explore t…

2014 Icarus
Cassini 64