Search Publications

Oxygen ion escape at Mars in a hybrid model: High energy and low energy ions
DOI: 10.1016/j.icarus.2009.05.015 Bibcode: 2010Icar..206..152K

Jarvinen, Riku; Kallio, Esa; Janhunen, Pekka +2 more

We have studied the escape and energization of several O+ populations and an O2+ population at Mars by using a hybrid model. The quasi-neutral hybrid model, HYB-Mars model, included five oxygen ion populations making it possible to distinguish photoions from oxygen ions originating from charge exchange processes and from the ionosphere.…

2010 Icarus
MEx 52
Clouds on Titan during the Cassini prime mission: A complete analysis of the VIMS data
DOI: 10.1016/j.icarus.2009.08.024 Bibcode: 2010Icar..205..571B

Brown, Michael E.; Schaller, Emily L.; Roberts, Jessica E.

We use data from the VIMS instrument on board the Cassini spacecraft to construct high sensitivity and high spatial-resolution maps of the locations of tropospheric clouds on Titan in the late northern winter season during which the Cassini prime mission took place. These observations show that, in this season, clouds on Titan are strongly hemisph…

2010 Icarus
Cassini 51
Analysis of phyllosilicate deposits in the Nili Fossae region of Mars: Comparison of TES and OMEGA data
DOI: 10.1016/j.icarus.2009.09.006 Bibcode: 2010Icar..206..269M

Mangold, Nicolas; Bibring, Jean-Pierre; Poulet, François +1 more

Diverse phyllosilicate deposits discovered previously in the Nili Fossae region with near infrared reflectance data are a window into the complex history of aqueous alteration on Mars. In this work, we used thermal infrared data from the Thermal Emission Spectrometer (TES) in combination with near infrared data from the Observatoire pour la Minéra…

2010 Icarus
MEx 51
Distribution and evolution of scalloped terrain in the southern hemisphere, Mars
DOI: 10.1016/j.icarus.2009.09.010 Bibcode: 2010Icar..206..691Z

Reiss, Dennis; Neukum, Gerhard; Hauber, Ernst +2 more

Scalloped depressions are a unique martian surface morphology found in the northern and southern hemisphere latitude-dependent dust and ice-rich surface mantles. These features exhibit a distinct asymmetric north-south slope profile, characterized by steep pole-facing scarps, flat floors and gentle equator-facing slopes. We examined High Resolutio…

2010 Icarus
MEx 49
Radar-bright channels on Titan
DOI: 10.1016/j.icarus.2009.12.027 Bibcode: 2010Icar..207..948L

Lorenz, R. D.; Janssen, M. A.; Cassini RADAR Team +3 more

During Cassini's T44 flyby of Titan (May 28, 2008), the Cassini SAR (synthetic aperture radar) revealed sinuous channels in the Southwest of Xanadu. These channels feature very large radar cross-sections, up to 5 dB, whereas the angle of incidence was relatively high, ∼20°. This backscatter is larger than allowed by the coherent backscatter model …

2010 Icarus
Cassini 49
Molecular hydrogen in Titan’s atmosphere: Implications of the measured tropospheric and thermospheric mole fractions
DOI: 10.1016/j.icarus.2010.03.003 Bibcode: 2010Icar..208..878S

Strobel, Darrell F.

The third most abundant species in Titan's atmosphere is molecular hydrogen with a tropospheric/lower stratospheric mole fraction of 0.001 derived from Voyager and Cassini infrared measurements. The globally averaged thermospheric H mole fraction profile from the Cassini Ion Neutral Mass Spectrometer (INMS) measurements implies a small positive gr…

2010 Icarus
Cassini 48
Geology of the Selk crater region on Titan from Cassini VIMS observations
DOI: 10.1016/j.icarus.2010.03.001 Bibcode: 2010Icar..208..905S

Nicholson, Philip D.; Sotin, Christophe; Barnes, Jason W. +9 more

Observations of Titan obtained by the Cassini Visual and Infrared Mapping Spectrometer (VIMS) have revealed Selk crater, a geologically young, bright-rimmed, impact crater located ∼800 km north-northwest of the Huygens landing site. The crater rim-crest diameter is ∼90 km; its floor diameter is ∼60 km. A central pit/peak, 20-30 km in diameter, is …

2010 Icarus
Cassini 48
The ultraviolet reflectance of Enceladus: Implications for surface composition
DOI: 10.1016/j.icarus.2009.11.007 Bibcode: 2010Icar..206..608H

Hendrix, Amanda R.; Hansen, Candice J.; Holsclaw, Greg M.

The reflectance of Saturn's moon Enceladus has been measured at far ultraviolet (FUV) wavelengths (115-190 nm) by Cassini's Ultraviolet Imaging Spectrograph (UVIS). At visible and near infrared (VNIR) wavelengths Enceladus' reflectance spectrum is very bright, consistent with a surface composed primarily of H 2O ice. At FUV wavelengths,…

2010 Icarus
Cassini eHST 48
Dayside induced magnetic field in the ionosphere of Mars
DOI: 10.1016/j.icarus.2009.03.021 Bibcode: 2010Icar..206..104A

Gurnett, D. A.; Morgan, D. D.; Modolo, R. +5 more

The Mars Advanced Radar for Subsurface and Ionospheric Sounding (MARSIS) onboard the Mars Express spacecraft has occasionally displayed surprising features. One such feature is the occurrence of a series of broadband, low-frequency echoes at equally spaced delay times after the sounder transmitter pulse. The interval between the echoes has been sh…

2010 Icarus
MEx 48
Estimating the masses of Saturn’s A and B rings from high-optical depth N-body simulations and stellar occultations
DOI: 10.1016/j.icarus.2009.09.012 Bibcode: 2010Icar..206..431R

Colwell, Joshua E.; Sremčević, Miodrag; Robbins, Stuart J. +2 more

We have completed a series of local N-body simulations of Saturn's B and A rings in order to identify systematic differences in the degree of particle clumping into self-gravity wakes as a function of orbital distance from Saturn and dynamical optical depth (a function of surface density). These simulations revealed that the normal optical depth o…

2010 Icarus
Cassini 47