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Venus Express observations of ULF and ELF waves in the Venus ionosphere: Wave properties and sources
DOI: 10.1016/j.icarus.2013.08.019 Bibcode: 2013Icar..226.1527R

Russell, C. T.; Wei, H. Y.; Zhang, T. L. +3 more

Electrical activity in a planetary atmosphere enables chemical reactions that are not possible under conditions of local thermodynamic equilibrium. In both the Venus and terrestrial atmospheres, lightning forms nitric oxide. Despite the existence of an inventory of NO at Venus like the Earth’s, and despite observations of the signals expected from…

2013 Icarus
VenusExpress 12
The opposition effect in Saturn’s main rings as seen by Cassini ISS: 1. Morphology of phase functions and dependence on the local optical depth
DOI: 10.1016/j.icarus.2013.01.015 Bibcode: 2013Icar..226..591D

Déau, Estelle; Dones, Luke; Charnoz, Sébastien +4 more

During the Prime mission (2004-2008), the Cassini cameras captured the opposition effect in Saturn’s main rings with a fine radial resolution at extremely small phase angles. Phase functions were extracted for 211 different radial locations in the main ring system (135 in the broadband clear filter of the Wide Angle Camera at 635 nm, 76 in four na…

2013 Icarus
Cassini 12
Upper limits for PH3 and H2S in Titan's atmosphere from Cassini CIRS
DOI: 10.1016/j.icarus.2013.02.024 Bibcode: 2013Icar..224..253N

Nixon, Conor A.; Irwin, Patrick G. J.; Teanby, Nicholas A. +1 more

We have searched for the presence of simple P and S-bearing molecules in Titan's atmosphere, by looking for the characteristic signatures of phosphine and hydrogen sulfide in infrared spectra obtained by Cassini CIRS. As a result we have placed the first upper limits on the stratospheric abundances, which are 1 ppb (PH3) and 330 ppb (H<…

2013 Icarus
Cassini 12
Earliest recorded ground-based decameter wavelength observations of Saturn's lightning during the giant E-storm detected by Cassini spacecraft in early 2006
DOI: 10.1016/j.icarus.2012.07.024 Bibcode: 2013Icar..224...14K

Gurnett, D. A.; Kurth, W. S.; Rucker, H. O. +12 more

We report the history of the first recorded ground-based radio detection of Saturn's lightning using the Ukrainian UTR-2 radiotelescope at frequencies from 20 to 25 MHz. The observations were performed between 29 January and 3 February 2006, during which lighting activity (E-storm) on Saturn was detected by the radio experiment onboard Cassini spa…

2013 Icarus
Cassini 12
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