Search Publications

Mars exospheric thermal and non-thermal components: Seasonal and local variations
DOI: 10.1016/j.icarus.2012.07.022 Bibcode: 2012Icar..221..682Y

Leblanc, F.; Modolo, R.; Hess, S. +3 more

A model of the martian exosphere is built for average solar conditions. A Chamberlain’s approach (Chamberlain, J.W. [1963]. Planet. Space Sci. 11, 901) is used to describe the O, CO, CO2, and O2 thermal exospheric components. The average thermal oxygen density at 300 km in altitude varies by about one order of magnitude with …

2012 Icarus
MEx 49
Physical properties of trans-neptunian binaries (120347) Salacia-Actaea and (42355) Typhon-Echidna
DOI: 10.1016/j.icarus.2012.03.029 Bibcode: 2012Icar..219..676S

Buie, M. W.; Rieke, G. H.; Roe, H. G. +7 more

We report new Hubble Space Telescope and Spitzer Space Telescope results concerning the physical properties of the trans-neptunian object (TNO) binaries (120347) Salacia-Actaea (formerly 2004 SB60), and (42355) Typhon-Echidna (formerly 2002 CR46). The mass of the (120347) Salacia-Actaea system is 4.66 ± 0.22 × 1020

2012 Icarus
eHST 49
Enceladus: A hypothesis for bringing both heat and chemicals to the surface
DOI: 10.1016/j.icarus.2012.05.031 Bibcode: 2012Icar..221...53M

Matson, Dennis L.; Johnson, Torrence V.; Castillo-Rogez, Julie C. +1 more

The eruptive plumes and large heat flow (∼15 GW) observed by Cassini in the South Polar Region of Enceladus may be expressions of hydrothermal activity inside Enceladus. We hypothesize that a subsurface ocean is the heat reservoir for thermal anomalies on the surface and the source of heat and chemicals necessary for the plumes. The ocean is belie…

2012 Icarus
Cassini 48
Composition and structures of the subsurface in the vicinity of Valles Marineris as revealed by central uplifts of impact craters
DOI: 10.1016/j.icarus.2012.07.031 Bibcode: 2012Icar..221..436Q

Quantin, Cathy; Flahaut, Jessica; Clenet, Harold +2 more

Despite recent efforts from space exploration to sound the martian subsurface with RADAR, the structure of the martian subsurface is still unknown. Major geologic contacts or discontinuities inside the martian crust have not been revealed. Another way to analyze the subsurface is to study rocks that have been exhumed from depth by impact processes…

2012 Icarus
MEx 45
Radar properties of comets: Parametric dielectric modeling of Comet 67P/Churyumov-Gerasimenko
DOI: 10.1016/j.icarus.2012.09.023 Bibcode: 2012Icar..221..925H

Kofman, Wlodek; Heggy, Essam; Palmer, Elizabeth M. +3 more

In 2014, the European Space Agency’s Rosetta mission is scheduled to rendezvous with Comet 67P/Churyumov-Gerasimenko (Comet 67P). Rosetta’s CONSERT experiment aims to explore the cometary nucleus’ geophysical properties using radar tomography. The expected scientific return and inversion algorithms are mainly dependent on our understanding of the …

2012 Icarus
Rosetta 45
Constraints on mantle plumes on Venus: Implications for volatile history
DOI: 10.1016/j.icarus.2011.09.011 Bibcode: 2012Icar..217..510S

Sotin, Christophe; Smrekar, Suzanne E.

The analysis of Venus' gravity field and topography suggests the presence of a small number of deep mantle plumes (∼9). This study predicts the number of plumes formed at the core-mantle boundary, their characteristics, and the production of partial melt from adiabatic decompression. Numerical simulations are performed using a 3D spherical code th…

2012 Icarus
VenusExpress 45
Magnetosphere-atmosphere coupling at Saturn: 1 - Response of thermosphere and ionosphere to steady state polar forcing
DOI: 10.1016/j.icarus.2012.08.034 Bibcode: 2012Icar..221..481M

Galand, M.; Moore, L.; Müller-Wodarg, I. C. F. +2 more

We present comprehensive calculations of the steady state response of Saturn’s coupled thermosphere-ionosphere to forcing by solar radiation, magnetospheric energetic electron precipitation and high latitude electric fields caused by sub-corotation of magnetospheric plasma. Significant additions to the physical processes calculated in our Saturn T…

2012 Icarus
Cassini 42
Valleys, paleolakes and possible shorelines at the Libya Montes/Isidis boundary: Implications for the hydrologic evolution of Mars
DOI: 10.1016/j.icarus.2012.03.012 Bibcode: 2012Icar..219..393E

Poulet, F.; Jaumann, R.; Hiesinger, H. +5 more

We describe the results of our morphologic, stratigraphic and mineralogic investigations of fluvial landforms, paleolakes and possible shoreline morphologies at the Libya Montes/Isidis Planitia boundary. The landforms are indicative of aqueous activity and standing bodies of water, including lakes, seas and oceans, that are attributed to a complex…

2012 Icarus
MEx 42
Geologic interpretation of the near-infrared images of the surface taken by the Venus Monitoring Camera, Venus Express
DOI: 10.1016/j.icarus.2011.11.003 Bibcode: 2012Icar..217..434B

Scholten, F.; Roatsch, Th.; Fiethe, B. +9 more

We analyze night-time near-infrared (NIR) thermal emission images of the Venus surface obtained with the 1-µm channel of the Venus Monitoring Camera onboard Venus Express. Comparison with the results of the Magellan radar survey and the model NIR images of the Beta-Phoebe region show that the night-time VMC images provide reliable informatio…

2012 Icarus
VenusExpress 41
The abundance, vertical distribution and origin of H2O in Titan’s atmosphere: Herschel observations and photochemical modelling
DOI: 10.1016/j.icarus.2012.09.006 Bibcode: 2012Icar..221..753M

Hartogh, Paul; Lellouch, Emmanuel; Lara, Luisa M. +4 more

Disk-averaged observations of water vapor in Titan’s atmosphere acquired with the Herschel satellite are reported. We use a combination of unresolved measurements of three H2O rotational lines at 66.4, 75.4 and 108.0 µm with the PACS instrument, and spectrally-resolved observations of two other transitions at 557 GHz (538 µm…

2012 Icarus
Cassini Herschel ISO 41