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Morphology, stratigraphy, and mineralogical composition of a layered formation covering the plateaus around Valles Marineris, Mars: Implications for its geological history
DOI: 10.1016/j.icarus.2010.03.012 Bibcode: 2010Icar..208..684L

Le Mouélic, S.; Bibring, J. -P.; Jaumann, R. +5 more

An extensive layered formation covers the high plateaus around Valles Marineris. Mapping based on HiRISE, CTX and HRSC images reveals these layered deposits (LDs) crop out north of Tithonium Chasma, south of Ius Chasma, around West Candor Chasma, and southwest of Juventae Chasma and Ganges Chasma. The estimated area covered by LDs is ∼42,300 km

2010 Icarus
MEx 47
Negative ions in the Enceladus plume
DOI: 10.1016/j.icarus.2009.07.013 Bibcode: 2010Icar..206..618C

Lewis, G. R.; Coates, A. J.; Jones, G. H. +6 more

During Cassini's Enceladus encounter on 12th March 2008, the Cassini Electron Spectrometer, part of the CAPS instrument, detected fluxes of negative ions in the plumes from Enceladus. It is thought that these ions include negatively charged water group cluster ions associated with the plume and forming part of the 'plume ionosphere'. In this paper…

2010 Icarus
Cassini 47
Threshold of wave generation on Titan’s lakes and seas: Effect of viscosity and implications for Cassini observations
DOI: 10.1016/j.icarus.2009.12.004 Bibcode: 2010Icar..207..932L

Lorenz, Ralph D.; Lunine, Jonathan I.; Newman, Claire

Motivated by radar and near-infrared data indicating that Titan's polar lakes are extremely smooth, we consider the conditions under which a lake surface will be ruffled by wind to form capillary waves. We evaluate laboratory data on wind generation and derive, without scaling for surface tension effects, a threshold for pure methane/ethane of ∼0.…

2010 Icarus
Cassini 46
Magnetic anomalies near Apollinaris Patera and the Medusae Fossae Formation in Lucus Planum, Mars
DOI: 10.1016/j.icarus.2010.01.009 Bibcode: 2010Icar..208..118H

Williams, David A.; Langlais, Benoit; Poulet, Francois +3 more

The nature of strong martian crustal field sources is investigated by mapping and modeling of Mars Global Surveyor magnetometer data near Apollinaris Patera, a previously proposed volcanic source, supplemented by large-scale correlative studies. Regional mapping yields evidence for positive correlations of orbital anomalies with both Apollinaris P…

2010 Icarus
MEx 46
Venus night airglow: Ground-based detection of OH, observations of O 2 emissions, and photochemical model
DOI: 10.1016/j.icarus.2009.10.019 Bibcode: 2010Icar..207...17K

Krasnopolsky, Vladimir A.

Venus nightglow was observed at NASA IRTF using a high-resolution long-slit spectrograph CSHELL at LT = 21:30 and 4:00 on Venus. Variations of the O 2 airglow at 1.27 µm and its rotational temperature are extracted from the observed spectra. The mean O 2 nightglow is 0.57 MR at 21:30 at 35°S-35°N, and the temperature in…

2010 Icarus
VenusExpress 45
Compositional heterogeneity of Asteroid 4 Vesta’s southern hemisphere: Implications for the Dawn mission
DOI: 10.1016/j.icarus.2010.07.015 Bibcode: 2010Icar..210..693R

Nathues, Andreas; Li, Jian-Yang; Reddy, Vishnu +3 more

High signal-to-noise, rotationally-resolved spectra of Asteroid 4 Vesta's southern hemisphere from the 2007 opposition were used to constrain its compositional and mineralogical variations. The spectra were rotationally-phased using closely timed HST observations of Vesta by Li et al. (Li, J.-Y., McFadden, L.A., Thomas, P.C., Mutchler, M.J., Parke…

2010 Icarus
eHST 45
Simulating the density and thermal structure of the middle atmosphere (∼80-130 km) of Mars using the MGCM-MTGCM: A comparison with MEX/SPICAM observations
DOI: 10.1016/j.icarus.2009.06.034 Bibcode: 2010Icar..206....5M

Smith, M. D.; Forget, F.; Montmessin, F. +4 more

The objective of this work is to advance the understanding of the structure and dynamics of the middle altitude region of the martian atmosphere. While numerous advancements have been made in the level of scientific understanding of Mars's upper and lower atmospheres over the past several decades, insight into the mechanisms of the middle atmosphe…

2010 Icarus
MEx 43
The source of widespread 3-µm absorption in Jupiter’s clouds: Constraints from 2000 Cassini VIMS observations
DOI: 10.1016/j.icarus.2010.06.039 Bibcode: 2010Icar..210..230S

Sromovsky, L. A.; Fry, P. M.

The Cassini flyby of Jupiter in 2000 provided spatially resolved spectra of Jupiter's atmosphere using the Visual and Infrared Mapping Spectrometer (VIMS). A prominent characteristic of these spectra is the presence of a strong absorption at wavelengths from about 2.9 µm to 3.1 µm, previously noticed in a 3-µm spectrum obtained b…

2010 Icarus
Cassini ISO eHST 43
Indications of brine related local seepage phenomena on the northern hemisphere of Mars
DOI: 10.1016/j.icarus.2009.10.012 Bibcode: 2010Icar..207..149K

Möhlmann, D.; Kereszturi, A.; Berczi, Sz. +5 more

Springtime low albedo features, called Dark Dune Spots, on the seasonal frost covered dunes on Mars between 77°N and 84°N latitude have been analyzed. Two groups of these spots have been identified: "small" and "large" ones, where large spots have diameters above 4 m, and complex internal structure. From these "large" spots branching seepage-like …

2010 Icarus
MEx 43
Elastic ice shells of synchronous moons: Implications for cracks on Europa and non-synchronous rotation of Titan
DOI: 10.1016/j.icarus.2010.04.013 Bibcode: 2010Icar..209..631G

Goldreich, Peter M.; Mitchell, Jonathan L.

A number of synchronous moons are thought to harbor water oceans beneath their outer ice shells. A subsurface ocean frictionally decouples the shell from the interior. This has led to proposals that a weak tidal or atmospheric torque might cause the shell to rotate differentially with respect to the synchronously rotating interior. Applications al…

2010 Icarus
Cassini 42