Search Publications

Enceladus's measured physical libration requires a global subsurface ocean
DOI: 10.1016/j.icarus.2015.08.037 Bibcode: 2016Icar..264...37T

Burns, J. A.; Porco, C.; Tajeddine, R. +5 more

Several planetary satellites apparently have subsurface seas that are of great interest for, among other reasons, their possible habitability. The geologically diverse saturnian satellite Enceladus vigorously vents liquid water and vapor from fractures within a south polar depression and thus must have a liquid reservoir or active melting. However…

2016 Icarus
Cassini 297
Titan's surface at 2.18-cm wavelength imaged by the Cassini RADAR radiometer: Results and interpretations through the first ten years of observation
DOI: 10.1016/j.icarus.2015.09.027 Bibcode: 2016Icar..270..443J

Lorenz, R. D.; Janssen, M. A.; Hayes, A. G. +12 more

A comprehensive calibration and mapping of the thermal microwave emission from Titan's surface is reported based on radiometric data obtained at 2.18-cm wavelength by the passive radiometer included in the Cassini RADAR instrument. Compared to previous work, the present results incorporate the much larger data set obtained in the approximately ten…

2016 Icarus
Cassini 77
The B-ring's surface mass density from hidden density waves: Less than meets the eye?
DOI: 10.1016/j.icarus.2016.01.007 Bibcode: 2016Icar..279..109H

Nicholson, P. D.; Hedman, M. M.

Saturn's B ring is the most opaque ring in our Solar System, but many of its fundamental parameters, including its total mass, are not well constrained. Spiral density waves generated by mean-motion resonances with Saturn's moons provide some of the best constraints on the rings' mass density, but detecting and quantifying such waves in the B ring…

2016 Icarus
Cassini 52
Nature, distribution, and origin of Titan's Undifferentiated Plains
DOI: 10.1016/j.icarus.2015.11.034 Bibcode: 2016Icar..270..162L

Janssen, M. A.; Cassini RADAR Team; Lopes, Rosaly M. C. +15 more

The Undifferentiated Plains on Titan, first mapped by Lopes et al. (Lopes, R.M.C. et al., 2010. Icarus, 205, 540-588), are vast expanses of terrains that appear radar-dark and fairly uniform in Cassini Synthetic Aperture Radar (SAR) images. As a result, these terrains are often referred to as ;blandlands;. While the interpretation of several other…

2016 Icarus
Cassini 48
Alluvial Fan Morphology, distribution and formation on Titan
DOI: 10.1016/j.icarus.2016.02.013 Bibcode: 2016Icar..270..238B

Hayes, A. G.; Birch, S. P. D.; Radebaugh, J. +2 more

Titan is a hydrologically active world, with dozens of alluvial fans that are evidence of sediment transport from high to low elevations. However, the distribution and requirements for the formation of fans on Titan are not well understood. We performed the first global survey of alluvial fans on Titan using Cassini Synthetic Aperture Radar (SAR) …

2016 Icarus
Cassini 41
Titan's temporal evolution in stratospheric trace gases near the poles
DOI: 10.1016/j.icarus.2015.08.027 Bibcode: 2016Icar..270..409C

Nixon, Conor A.; Achterberg, Richard K.; Flasar, F. Michael +7 more

We analyze spectra acquired by the Cassini/Composite Infrared Spectrometer (CIRS) at high resolution from October 2010 until September 2014 in nadir mode. Up until mid 2012, Titan's Northern atmosphere exhibited the enriched chemical content found since the Voyager days (November 1980), with a peak around the Northern Spring Equinox (NSE) in 2009.…

2016 Icarus
Cassini 40
Geomorphological map of the Afekan Crater region, Titan: Terrain relationships in the equatorial and mid-latitude regions
DOI: 10.1016/j.icarus.2016.02.021 Bibcode: 2016Icar..270..130M

Soderblom, Jason M.; Lorenz, Ralph D.; Turtle, Elizabeth P. +12 more

We carried out geomorphological mapping in a mid-latitude area surrounding the Afekan Crater region on Titan. We used Cassini RADAR (Synthetic Aperture Radar mode) data as the basemap, supplemented by Cassini RADAR microwave emissivity, Imaging Science Subsystem (ISS) infrared data, Visual and Infrared Mapping Spectrometer (VIMS) spectral images, …

2016 Icarus
Cassini 40
Titan's "Magic Islands": Transient features in a hydrocarbon sea
DOI: 10.1016/j.icarus.2016.02.022 Bibcode: 2016Icar..271..338H

Soderblom, Jason M.; Lorenz, Ralph D.; Malaska, Michael J. +6 more

The region of Titan's hydrocarbon sea, Ligeia Mare, where transient bright features were previously discovered, was anomalously bright in the first of two more recent Cassini RADAR observations but not the second. Another transient bright feature in a different region of Ligeia Mare was also discovered in the first of the new observations. Here we…

2016 Icarus
Cassini 39
Rhea gravity field and interior modeling from Cassini data analysis
DOI: 10.1016/j.icarus.2015.09.022 Bibcode: 2016Icar..264..264T

Nimmo, Francis; Iess, Luciano; Jacobson, Robert A. +4 more

During its tour of the Saturn system, Cassini performed two close flybys of Rhea dedicated to gravity investigations, the first in November 2005 and the second in March 2013. This paper presents an estimation of Rhea's fully unconstrained quadrupole gravity field obtained from a joint multi-arc analysis of the two Cassini flybys.

Our best est…

2016 Icarus
Cassini 38
Cassini Imaging Science Subsystem observations of Titan's south polar cloud
DOI: 10.1016/j.icarus.2014.11.038 Bibcode: 2016Icar..270..399W

West, R. A.; Rannou, P.; Lavvas, P. +5 more

In May of 2012 images of Titan obtained by the Cassini Imaging Science Subsystem (ISS) showed a newly-formed cloud patch near the southern pole. The cloud has unusual morphology and texture suggesting that it is formed by condensation at an altitude much higher than expected for any of the known organics in Titan's atmosphere. We measured the alti…

2016 Icarus
Cassini 37