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Exposure age of Saturn's A and B rings, and the Cassini Division as suggested by their non-icy material content
DOI: 10.1016/j.icarus.2017.04.008 Bibcode: 2017Icar..294...14Z

Nicholson, P. D.; Janssen, M. A.; Hayes, A. G. +4 more

Saturn's rings are composed primarily of water ice with a small fraction of non-icy constituents that are likely both intrinsic and extrinsic in origin. The intrinsic material is thought to be characteristic of the ring progenitor, while the extrinsic material is derived from the continual stream of hypervelocity impacting micrometeoroids that pol…

2017 Icarus
Cassini 39
Sulfur dioxide in the Venus Atmosphere: II. Spatial and temporal variability
DOI: 10.1016/j.icarus.2017.05.001 Bibcode: 2017Icar..295....1V

Vandaele, A. C.; Robert, S.; Montmessin, F. +18 more

The vertical distribution of sulfur species in the Venus atmosphere has been investigated and discussed in Part I of this series of papers dealing with the variability of SO2 on Venus. In this second part, we focus our attention on the spatial (horizontal) and temporal variability exhibited by SO2. Appropriate data sets - SPI…

2017 Icarus
VenusExpress eHST 39
Compositional and structural constraints on the geologic history of eastern Tharsis Rise, Mars
DOI: 10.1016/j.icarus.2016.09.005 Bibcode: 2017Icar..284...43V

Murchie, S. L.; Viviano-Beck, C. E.; Beck, A. W. +1 more

Identification and mapping of distinct compositional units using high-resolution orbital imagery of the walls of Valles Marineris, Mars, provide key structural and environmental constraints on the geologic history of the eastern Tharsis Rise. Our results corroborate an overall vertical structure of the upper crust consistent with that inferred fro…

2017 Icarus
MEx 36
Thermal structure of the upper atmosphere of Venus simulated by a ground-to-thermosphere GCM
DOI: 10.1016/j.icarus.2016.09.016 Bibcode: 2017Icar..281...55G

López-Valverde, M. A.; Gilli, G.; González-Galindo, F. +5 more

We present here the thermal structure of the upper atmosphere of Venus predicted by a full self-consistent Venus General Circulation Model (VGCM) developed at Laboratoire de Météorologie Dynamique (LMD) and extended up to the thermosphere of the planet. Physical and photochemical processes relevant at those altitudes, plus a non-orographic GW para…

2017 Icarus
VenusExpress 35
The thermal structure of the Venus atmosphere: Intercomparison of Venus Express and ground based observations of vertical temperature and density profiles
DOI: 10.1016/j.icarus.2017.04.020 Bibcode: 2017Icar..294..124L

Montmessin, Franck; Tanga, Paolo; Tellmann, Silvia +30 more

The Venus International Reference Atmosphere (VIRA) model contains tabulated values of temperature and number densities obtained by the experiments on the Venera entry probes, Pioneer Venus Orbiter and multi-probe missions in the 1980s. The instruments on the recent Venus Express orbiter mission generated a significant amount of new observational …

2017 Icarus
VenusExpress 35
Mars sedimentary rock erosion rates constrained using crater counts, with applications to organic-matter preservation and to the global dust cycle
DOI: 10.1016/j.icarus.2016.10.010 Bibcode: 2017Icar..286..212K

Kite, Edwin S.; Mayer, David P.

Small-crater counts on Mars light-toned sedimentary rock are often inconsistent with any isochron; these data are usually plotted then ignored. We show (using an 18-HiRISE-image, > 104-crater dataset) that these non-isochron crater counts are often well-fit by a model where crater production is balanced by crater obliteration via ste…

2017 Icarus
MEx 35
Cassini microwave observations provide clues to the origin of Saturn's C ring
DOI: 10.1016/j.icarus.2016.07.020 Bibcode: 2017Icar..281..297Z

Nicholson, P. D.; Hedman, M. M.; Janssen, M. A. +6 more

Despite considerable study, Saturn's rings continue to challenge current theories for their provenance. Water ice comprises the bulk of Saturn's rings, yet it is the small fraction of non-icy material that is arguably more valuable in revealing clues about the system's origin and age. Herein, we present new measurements of the non-icy material fra…

2017 Icarus
Cassini 33
Noncircular features in Saturn's rings IV: Absolute radius scale and Saturn's pole direction
DOI: 10.1016/j.icarus.2017.02.007 Bibcode: 2017Icar..290...14F

Nicholson, Philip D.; French, Richard G.; McGhee-French, Colleen A. +6 more

We present a comprehensive solution for the geometry of Saturn's ring system, based on orbital fits to an extensive set of occultation observations of 122 individual ring edges and gaps. We begin with a restricted set of very high quality Cassini VIMS, UVIS, and RSS measurements for quasi-circular features in the C and B rings and the Cassini Divi…

2017 Icarus
Cassini eHST 33
Decadal timescale variability of the Enceladus plumes inferred from Cassini images
DOI: 10.1016/j.icarus.2016.09.018 Bibcode: 2017Icar..282..260I

Ingersoll, Andrew P.; Ewald, Shawn P.

The brightness of the Enceladus plumes varies with position in the satellite's eccentric orbit, with altitude above the surface, and with time from one year to the next. Hedman et al. (2013, hereinafter H13) were the first to report these variations. They used data from Cassini's Visible and Infrared Mapping Spectrometer (VIMS). Here we present br…

2017 Icarus
Cassini 33
The near-surface methane humidity on Titan
DOI: 10.1016/j.icarus.2016.10.012 Bibcode: 2017Icar..286..270L

Lora, Juan M.; Ádámkovics, Máté

We retrieve vertical and meridional variations of methane mole fraction in Titan's lower troposphere by re-analyzing near-infrared ground-based observations from 17 July 2014 UT (Ádámkovics et al., 2016). We generate synthetic spectra using atmospheric methane profiles that do not contain supersaturation or discontinuities to fit the observations,…

2017 Icarus
Huygens 32