Search Publications

Titan’s internal structure and the evolutionary consequences
DOI: 10.1016/j.pss.2011.04.010 Bibcode: 2012P&SS...60...10F

Fortes, A. D.

Titan’s moment of inertia (MoI), estimated from the quadrupole gravity field measured by the Cassini spacecraft, is 0.342, which has been interpreted as evidence of a partially differentiated internal mass distribution. It is shown here that the observed MoI is equally consistent with a fully differentiated internal structure comprising a shell of…

2012 Planetary and Space Science
Cassini 79
Titan’s global crater population: A new assessment
DOI: 10.1016/j.pss.2011.02.016 Bibcode: 2012P&SS...60...26N

Lorenz, R. D.; Neish, C. D.

We report a revised crater population for Titan using Cassini RADAR data through January 2010 (flyby T65), and make a size-dependent correction for the incomplete coverage (∼33%) using a Monte-Carlo model. Qualitatively, Titan’s landscape is more heavily cratered than Earth, but much less than Mars or Ganymede: the area fraction covered by craters…

2012 Planetary and Space Science
Cassini 76
Titan's fluvial valleys: Morphology, distribution, and spectral properties
DOI: 10.1016/j.pss.2011.01.020 Bibcode: 2012P&SS...60...34L

Sotin, C.; Barnes, J. W.; Brown, R. H. +11 more

Titan's fluvial channels have been investigated based on data obtained by the Synthetic Aperture Radar (SAR) instrument and the Visible and Infrared Mapping Spectrometer (VIMS) onboard the Cassini spacecraft. In this paper, a database of fluvial features is created based on radar-SAR data aiming to unveil the distribution and the morphologic and s…

2012 Planetary and Space Science
Cassini 69
Spatial and temporal variations in Titan's surface temperatures from Cassini CIRS observations
DOI: 10.1016/j.pss.2011.03.015 Bibcode: 2012P&SS...60...62C

Irwin, P. G. J.; Teanby, N. A.; de Kok, R. +4 more

We report a wide-ranging study of Titan's surface temperatures by analysis of the Moon's outgoing radiance through a spectral window in the thermal infrared at 19 µm (530 cm-1) characterized by lower atmospheric opacity. We begin by modeling Cassini Composite Infrared Spectrometer (CIRS) far infrared spectra collected in the perio…

2012 Planetary and Space Science
Cassini 60
The Saturnian satellite Rhea as seen by Cassini VIMS
DOI: 10.1016/j.pss.2011.07.019 Bibcode: 2012P&SS...61..142S

Baines, Kevin H.; Buratti, Bonnie J.; Clark, Roger N. +16 more

Since the arrival of the Cassini spacecraft at Saturn in June 2004, the Visual and Infrared Mapping Spectrometer has obtained new spectral data of the icy satellites of Saturn in the spectral range from 0.35 to 5.2 µm. Numerous flybys were performed at Saturn’s second largest satellite Rhea, providing a nearly complete coverage with pixel-gr…

2012 Planetary and Space Science
Cassini 53
Ion densities and velocities in the inner plasma torus of Saturn
DOI: 10.1016/j.pss.2012.09.016 Bibcode: 2012P&SS...73..151H

Persoon, A. M.; Wahlund, J. -E.; Morooka, M. W. +1 more

We present plasma data from the Cassini Radio and Plasma Wave Science (RPWS) Langmuir probe (LP), mapping the ion density and velocity of Saturn's inner plasma torus. Data from 129 orbits, recorded during the period from the 1st of February 2005 to the 27th of June 2010, are used to map the extension of the inner plasma torus. The dominant part of…

2012 Planetary and Space Science
Cassini 38
Energetic charged particle weathering of Saturn's inner satellites
DOI: 10.1016/j.pss.2011.02.012 Bibcode: 2012P&SS...61...60P

Krupp, N.; Roussos, E.; Hendrix, A. R. +9 more

We characterize the relative importance of energetic electrons and protons to the weathering of five of the inner satellites of Saturn. To do this, we present data from the Magnetospheric Imaging Instrument on the Cassini spacecraft, some of which is averaged over the whole mission to date. We also compute averaged proton and electron energy spect…

2012 Planetary and Space Science
Cassini 37
Titan's lakes chemical composition: Sources of uncertainties and variability
DOI: 10.1016/j.pss.2011.05.009 Bibcode: 2012P&SS...61...99C

Lunine, J. I.; Cordier, D.; Mousis, O. +5 more

Between 2004 and 2007 the instruments of the Cassini spacecraft, orbiting within the Saturn system, discovered dark patches in the polar regions of Titan. These features are interpreted as hydrocarbon lakes and seas with ethane and methane identified as the main compounds. In this context, we have developed a lake-atmosphere equilibrium model allo…

2012 Planetary and Space Science
Cassini 36
Surface waves on Saturn's magnetopause
DOI: 10.1016/j.pss.2012.02.007 Bibcode: 2012P&SS...65..109M

Coates, A. J.; Dougherty, M. K.; Jones, G. H. +3 more

Waves on the surface of a planetary magnetopause promote energy transport into the magnetosphere, representing an important aspect of solar wind-magnetosphere coupling. At Saturn's magnetopause it has been proposed that growth of the Kelvin-Helmholtz (K-H) instability produces greater wave activity on the dawn side of the surface than on the dusk …

2012 Planetary and Space Science
Cassini 35
Dissipation of Titan's north polar cloud at northern spring equinox
DOI: 10.1016/j.pss.2011.04.006 Bibcode: 2012P&SS...60...86L

Nicholson, Philip D.; Sotin, Christophe; Barnes, Jason W. +10 more

Saturn's Moon Titan has a thick atmosphere with a meteorological cycle. We report on the evolution of the giant cloud system covering its north pole using observations acquired by the Visual and Infrared Mapping Spectrometer onboard the Cassini spacecraft. A radiative transfer model in spherical geometry shows that the clouds are found at an altit…

2012 Planetary and Space Science
Cassini 33