Search Publications

The geological history of Northeast Syrtis Major, Mars
DOI: 10.1016/j.icarus.2017.03.030 Bibcode: 2017Icar..293...66B

Mustard, John F.; Bramble, Michael S.; Salvatore, Mark R.

As inferred from orbital spectroscopic data, Northeast Syrtis Major bears considerable mineral diversity that spans the Noachian-Hesperian boundary despite its small geographic area. In this study we use observations from the High Resolution Imaging Science Experiment, supplemented with Context Camera imagery, to characterize and map the lateral e…

2017 Icarus
MEx 55
Sulfur dioxide in the Venus atmosphere: I. Vertical distribution and variability
DOI: 10.1016/j.icarus.2017.05.003 Bibcode: 2017Icar..295...16V

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

Recent observations of sulfur containing species (SO2, SO, OCS, and H2SO4) in Venus' mesosphere have generated controversy and great interest in the scientific community. These observations revealed unexpected spatial patterns and spatial/temporal variability that have not been satisfactorily explained by models. S…

2017 Icarus
VenusExpress 54
True polar wander of Enceladus from topographic data
DOI: 10.1016/j.icarus.2017.04.019 Bibcode: 2017Icar..295...46T

Hedman, Matthew M.; Schenk, Paul M.; Burns, Joseph A. +4 more

Many objects in the solar system are suspected to have experienced reorientation of their spin axes. As their rotation rates are slow and their shapes are nearly spherical, the formation of mass anomalies, by either endogenic or exogenic processes, can change objects' moments of inertia. Therefore, the objects reorient to align their largest momen…

2017 Icarus
Cassini 46
Impact crater relaxation on Dione and Tethys and relation to past heat flow
DOI: 10.1016/j.icarus.2017.01.025 Bibcode: 2017Icar..288...37W

Schenk, Paul M.; White, Oliver L.; Bray, Veronica J. +3 more

Relating relaxation of impact crater topography to past heat flow through the crusts of icy satellites is a technique that has been applied to satellites around Jupiter and Saturn. We use global digital elevation models of the surfaces of Dione and Tethys generated from Cassini data to obtain crater depth/diameter (d/D) data. Relaxation is found t…

2017 Icarus
Cassini 43
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