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Patterned ground in martian high northern latitudes: Morphology and age constraints
DOI: 10.1016/j.icarus.2012.09.032 Bibcode: 2013Icar..225..960K

Korteniemi, J.; Kreslavsky, M. A.

We performed a systematic survey of typical surface patterns and small (5-50 m) impact craters in a zone between 50° and 70° latitude in the Northern Lowlands of Mars. We found that small-scale (<10 m) polygonal pattern formed by narrow fractures is typical in the northern half of the studied zone. We interpret this pattern to be formed by acti…

2013 Icarus
MEx 11
Comparative analysis of airglow emissions in terrestrial planets, observed with VIRTIS-M instruments on board Rosetta and Venus Express
DOI: 10.1016/j.icarus.2013.07.027 Bibcode: 2013Icar..226.1115M

Piccioni, G.; Capaccioni, F.; Gérard, J. -C. +3 more

Airglow emissions are optimal processes to investigate the chemistry and dynamics in planetary atmospheres. In this study, we focus on the O2 and OH airglow emissions in Venus, Earth, and Mars atmospheres, which are controlled by chemical reactions common to the three planets. By studying these phenomena on Venus, Earth, and Mars using …

2013 Icarus
Rosetta VenusExpress 11
Temperature and variability of Pillan, Wayland Patera, and Loki Patera on Io from Cassini ISS data
DOI: 10.1016/j.icarus.2013.05.026 Bibcode: 2013Icar..226...77A

Radebaugh, Jani; Stephens, Denise C.; Allen, Daniel R.

Cassini spacecraft images of Io obtained during its flyby of Jupiter in late 2000 and early 2001 were used to determine the lava composition and eruption style of three faint hot spots, Pillan, Wayland Patera, and Loki Patera. We found a maximum color temperature of 1130 ± 289 K for Pillan and maximum color temperatures of 1297 ± 289 K and 1387 ± …

2013 Icarus
Cassini 11
Age and evolution of the lower NW flank of the Hecates Tholus volcano, Mars, based on crater size-frequency distribution on CTX images
DOI: 10.1016/j.icarus.2013.05.012 Bibcode: 2013Icar..226..455D

Michael, G. G.; de Pablo, M. A.; Centeno, J. D.

We present results of crater size-frequency distribution (SFD) analysis of the lower NW flank of the Hecates Tholus volcano, Elysium volcanic province of Mars, by the use of images acquired by the Context (CTX) instrument on board of Mars Reconnaissance Orbiter (6 m/pixel in resolution). Previous similar works were focused on the caldera complex o…

2013 Icarus
MEx 10
Comparison of general circulation model atmospheric wave simulations with wind observations of venusian mesosphere
DOI: 10.1016/j.icarus.2013.02.029 Bibcode: 2013Icar..225..840N

Aoki, Shohei; Kasaba, Yasumasa; Nakagawa, Hiromu +5 more

Simulations from our venusian general circulation model (GCM) forcing the presence of planetary-scale waves and mesoscale gravity waves were compared with infrared (IR) heterodyne observations of Doppler wind velocities in the venusian mesospheric altitude region (110 km). Observations confirmed the strong short-term variations in the venusian mes…

2013 Icarus
VenusExpress 9
Titan's Xanadu region: Geomorphology and formation scenario
DOI: 10.1016/j.icarus.2013.01.016 Bibcode: 2013Icar..223..796L

Lunine, Jonathan I.; Mitri, Giuseppe; Langhans, Migrjam

Based on comprehensive mapping of the region, the recent theories of Xanadu's origin are examined and a chronology of geologic processes is proposed. The geologic history of Titan's Xanadu region is different from that of the other surface units on Saturn's moon. A previously proposed origin of western Xanadu from a giant impact in the early histo…

2013 Icarus
Cassini 9
Remote sensing of the energy of auroral electrons in Saturn’s atmosphere: Hubble and Cassini spectral observations
DOI: 10.1016/j.icarus.2012.11.033 Bibcode: 2013Icar..223..211G

Bonfond, B.; Nichols, J. D.; Clarke, J. T. +6 more

Saturn’s north ultraviolet aurora has been successfully observed twice between March and May 2011 with the STIS long-slit spectrograph on board the Hubble Space Telescope. Spatially resolved spectra at ∼12 Å spectral resolution have been collected at different local times from dawn to dusk to determine the amount of hydrocarbon absorption. For thi…

2013 Icarus
Cassini eHST 9
Evidence for Amazonian mid-latitude glaciation on Mars from impact crater asymmetry
DOI: 10.1016/j.icarus.2013.04.013 Bibcode: 2013Icar..225..413C

Mangold, Nicolas; Conway, Susan J.

We find that crater slopes in the mid-latitudes of Mars have a marked north-south asymmetry, with the pole-facing slopes being shallower. We mapped impact craters in two southern hemisphere sites (Terra Cimmeria and Noachis Terra) and one northern hemisphere site (Acidalia Planitia) and used elevation data from the High Resolution Stereo Camera (H…

2013 Icarus
MEx 9
The dark side of Saturn’s B ring: Seasons as clues to its structure
DOI: 10.1016/j.icarus.2012.12.006 Bibcode: 2013Icar..223...28F

Ferrari, C.; Reffet, E.

The unlit side of the dense B ring of Saturn does not receive direct sunlight. Yet it cools down as the Sun sets on the ring from solstice to equinox. A multi-scale thermal model that treats the heat transfer through a packed ensemble of particles is built to study the orbital and seasonal temperature variations of both lit and unlit sides of this…

2013 Icarus
Cassini 8
Retrieval of jovian cloud structure from the Cassini ISS limb-darkening data. I. Continuum scattering phase functions for cloud and haze in the South Tropical Zone
DOI: 10.1016/j.icarus.2012.09.035 Bibcode: 2013Icar..222..100S

Kasaba, Y.; Sato, T. M.; Satoh, T.

We have deduced the scattering properties of aerosols in the jovian upper troposphere by analyzing imaging data obtained at a wide variety of solar phase angles (4-140°) by the Cassini Imaging Science Subsystem (ISS) Narrow Angle Camera (NAC) during its flyby of Jupiter. The limb-darkening curves along the South Tropical Zone (STrZ) are extracted …

2013 Icarus
Cassini 8