Search Publications

Nitrile gas chemistry in Titan's atmosphere
DOI: 10.1016/j.icarus.2011.04.005 Bibcode: 2011Icar..213..625G

Gautier, Thomas; Carrasco, Nathalie; Szopa, Cyril +3 more

This work presents the first study of the gaseous products resulting from the partial dissociation of methane and nitrogen in the PAMPRE experimental setup simulating Titan's atmospheric chemistry. Using cryogenic trapping, the gaseous products generated from the chemical reactions occurring in the reactor have been trapped. Analyses of these prod…

2011 Icarus
Cassini 67
Five new and three improved mutual orbits of transneptunian binaries
DOI: 10.1016/j.icarus.2011.03.012 Bibcode: 2011Icar..213..678G

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

We present three improved and five new mutual orbits of transneptunian binary systems (58534) Logos-Zoe, (66652) Borasisi-Pabu, (88611) Teharonhiawako-Sawiskera, (123509) 2000 WK 183, (149780) Altjira, 2001 QY 297, 2003 QW 111, and 2003 QY 90 based on Hubble Space Telescope and Keck II laser guide star a…

2011 Icarus
eHST 66
Evidence for weathering on early Mars from a comparison with terrestrial weathering profiles
DOI: 10.1016/j.icarus.2011.09.004 Bibcode: 2011Icar..216..257G

Mangold, N.; Dehouck, E.; Gaudin, A.

Phyllosilicates on Mars are widespread in the ancient crust suggesting the presence of liquid water at the martian surface and therefore warmer conditions during its early history. However, the role of the ancient climate in the alteration process, which produced these phyllosilicates, remains under debate, because similar mineral assemblages can …

2011 Icarus
MEx 64
Titan: An exogenic world?
DOI: 10.1016/j.icarus.2011.01.019 Bibcode: 2011Icar..212..790M

Moore, Jeffrey M.; Pappalardo, Robert T.

All landforms on Titan that are unambiguously identifiable can be explained by exogenic processes (aeolian, fluvial, impact cratering, and mass wasting). Previous suggestions of endogenically produced cryovolcanic constructs and flows have, without exception, lacked conclusive diagnostic evidence. The modification of sparse recognizable impact cra…

2011 Icarus
Cassini 64
An investigation of the SO 2 content of the venusian mesosphere using SPICAV-UV in nadir mode
DOI: 10.1016/j.icarus.2010.08.021 Bibcode: 2011Icar..211...58M

Montmessin, Franck; Bertaux, Jean-Loup; Marcq, Emmanuel +4 more

Using the SPICAV-UV spectrometer aboard Venus Express in nadir mode, we were able to derive spectral radiance factors in the middle atmosphere of Venus in the 170-320 nm range at a spectral resolution of R ≃ 200 during 2006 and 2007 in the northern hemisphere. By comparison with a radiative transfer model of the upper atmosphere of Venus, we could…

2011 Icarus
VenusExpress 64
UV and IR auroral emission model for the outer planets: Jupiter and Saturn comparison
DOI: 10.1016/j.icarus.2011.04.001 Bibcode: 2011Icar..213..581T

Fujimoto, Masaki; Badman, Sarah V.; Tao, Chihiro

Planetary aurora display the dynamic behavior of the plasma gas surrounding a planet. The outer planetary aurora are most often observed in the ultraviolet (UV) and the infrared (IR) wavelengths. How the emissions in these different wavelengths are connected with the background physical conditions are not yet well understood. Here we investigate t…

2011 Icarus
Cassini 61
Tidal dynamical considerations constrain the state of an ocean on Enceladus
DOI: 10.1016/j.icarus.2010.10.007 Bibcode: 2011Icar..211..770T

Tyler, R.

In previous work, solutions to the non-dissipative Laplace Tidal Equations (LTE) were used to provide bounds on the heat generated by the response of a subsurface ocean on Enceladus to an obliquity component of tidal forces. Here we improve these bounds using solutions from the LTE with a generic dissipation term explicitly added. We find solution…

2011 Icarus
Cassini 60
Condensation in Titan's atmosphere at the Huygens landing site
DOI: 10.1016/j.icarus.2011.06.040 Bibcode: 2011Icar..215..732L

Yelle, R. V.; Lavvas, P.; Griffith, C. A.

We present a self-consistent description of Titan's aerosols-clouds-gases system and compare our results with the optical properties retrieved from measurements made by the Descent Imager/Spectral Radiometer (DISR) experiment on the Huygens probe (Tomasko, M.G. et al. [2008]. Planet. Space Sci. 56, 669-707). Our calculations include the condensati…

2011 Icarus
Huygens 59
A high-amplitude thermal inertia anomaly of probable magnetospheric origin on Saturn's moon Mimas
DOI: 10.1016/j.icarus.2011.09.007 Bibcode: 2011Icar..216..221H

Johnson, R. E.; Paranicas, C.; Spencer, J. R. +5 more

Spectral maps of Mimas' daytime thermal emission show a previously unobserved thermal anomaly on Mimas' surface. A sharp V-shaped boundary, centered at 0°N and 180°W, separates relatively warm daytime temperatures from a cooler anomalous region occupying low- to mid-latitudes on the leading hemisphere. Subsequent observations show the anomalous re…

2011 Icarus
Cassini 58
Regional geomorphology and history of Titan's Xanadu province
DOI: 10.1016/j.icarus.2010.07.022 Bibcode: 2011Icar..211..672R

Lorenz, R. D.; West, R. D.; Stiles, B. +19 more

Titan's enigmatic Xanadu province has been seen in some detail with instruments from the Cassini spacecraft. The region contains some of the most rugged, mountainous terrain on Titan, with relief over 2000 m. Xanadu contains evolved and integrated river channels, impact craters, and dry basins filled with smooth, radar-dark material, perhaps sedim…

2011 Icarus
Cassini 58