Search Publications

On the thermal electron balance in Titan’s sunlit upper atmosphere
DOI: 10.1016/j.icarus.2012.12.010 Bibcode: 2013Icar..223..234V

Strobel, D. F.; Wahlund, J. -E.; Ågren, K. +8 more

The Cassini mission has investigated Titan’s upper atmosphere in detail and found that, under solar irradiation, it has a well-developed ionosphere, which peaks between 1000 and 1200 km. In this paper we focus on the T40, T41, T42 and T48 Titan flybys by the Cassini spacecraft and use in situ measurements of N2 and CH4 densit…

2013 Icarus
Cassini 34
Meteorology of Jupiter's equatorial hot spots and plumes from Cassini
DOI: 10.1016/j.icarus.2013.02.001 Bibcode: 2013Icar..223..832C

Showman, Adam P.; Simon-Miller, Amy A.; Vasavada, Ashwin R. +1 more

We present an updated analysis of Jupiter's equatorial meteorology from Cassini observations. For two months preceding the spacecraft's closest approach, the Imaging Science Subsystem (ISS) onboard regularly imaged the atmosphere. We created time-lapse movies from this period in order to analyze the dynamics of equatorial hot spots and their inter…

2013 Icarus
Cassini 34
Saturn’s visible lightning, its radio emissions, and the structure of the 2009-2011 lightning storms
DOI: 10.1016/j.icarus.2013.07.013 Bibcode: 2013Icar..226.1020D

Porco, Carolyn C.; Dyudina, Ulyana A.; Ingersoll, Andrew P. +3 more

Visible lightning on Saturn was first detected by the Cassini camera in 2009 at ∼35° South latitude. We report more lightning observations at ∼35° South later in 2009, and lightning in the 2010-2011 giant lightning storm at ∼35° North. The 2009 lightning is detected on the night side of Saturn in a broadband clear filter. The 2011 lightning is det…

2013 Icarus
Cassini 33
Saturn’s thermal emission at 2.2-cm wavelength as imaged by the Cassini RADAR radiometer
DOI: 10.1016/j.icarus.2013.06.008 Bibcode: 2013Icar..226..522J

Baines, K. H.; Edgington, S. G.; Janssen, M. A. +7 more

We present well-calibrated, high-resolution maps of Saturn’s thermal emission at 2.2-cm wavelength obtained by the Cassini RADAR radiometer through the Prime and Equinox Cassini missions, a period covering approximately 6 years. The absolute brightness temperature calibration of 2% achieved is more than twice better than for all previous microwave…

2013 Icarus
Cassini 32
Dications and thermal ions in planetary atmospheric escape
DOI: 10.1016/j.icarus.2012.09.034 Bibcode: 2013Icar..222..169L

Simon Wedlund, C.; Ehrenreich, D.; Witasse, O. +4 more

In the recent years, the presence of dications in the atmospheres of Mars, Venus, Earth and Titan has been modeled and assessed. These studies also suggested that these ions could participate to the escape of the planetary atmospheres because a large fraction of them is unstable and highly energetic. When they dissociate, their internal energy is …

2013 Icarus
MEx VenusExpress 31
The density and temperature structure near the exobase of Saturn from Cassini UVIS solar occultations
DOI: 10.1016/j.icarus.2013.07.037 Bibcode: 2013Icar..226.1318K

Sandel, B. R.; Yelle, R. V.; Koskinen, T. T. +4 more

We analyzed 15 solar occultations observed by the Cassini UVIS instrument to constrain the density and temperature structure near the exobase of Saturn. We retrieved the density of H2 and thus the temperature at altitudes higher than 1900 km above the 1 bar level by analyzing the ionization continuum of H2 at wavelengths shor…

2013 Icarus
Cassini 31
Comparing Dawn, Hubble Space Telescope, and ground-based interpretations of (4) Vesta
DOI: 10.1016/j.icarus.2013.07.019 Bibcode: 2013Icar..226.1103R

Nathues, Andreas; Russell, Christopher T.; Li, Jian-Yang +10 more

Observations of Asteroid (4) Vesta by NASA’s Dawn spacecraft are interesting because its surface has the largest range of albedo, color and composition of any other asteroid visited by spacecraft to date. These hemispherical and rotational variations in surface brightness and composition have been attributed to impact processes since Vesta’s forma…

2013 Icarus
eHST 28
Mineralogy of Mare Serenitatis on the near side of the Moon based on Chandrayaan-1 Moon Mineralogy Mapper (M3) observations
DOI: 10.1016/j.icarus.2012.10.020 Bibcode: 2013Icar..222..137K

Bhattacharya, Satadru; Chauhan, Prakash; Kiran Kumar, A. S. +2 more

Spectral analysis of Mare Serenitatis has been carried out using Chandrayaan-1 Moon Mineralogy Mapper (M3) data in order to map the compositional diversity of the basaltic units that exist in the basin. Mare Serenitatis is characterized by multiple basaltic flows of different ages indicating a prolonged volcanism subsequent to the basin…

2013 Icarus
Chandrayaan-1 27
Impact of tidal heating on the onset of convection in Enceladus’s ice shell
DOI: 10.1016/j.icarus.2013.06.033 Bibcode: 2013Icar..226..898B

Čadek, Ondřej; Tobie, Gabriel; Běhounková, Marie +1 more

By performing 3D simulations of thermal convection and tidal dissipation, we investigated the effect of tidal heating on the onset of convection in Enceladus’s ice shell. We considered a composite non-Newtonian rheology including diffusion, grain-size-sensitive and dislocation creeps, and we defined an effective tidal viscosity reproducing the dis…

2013 Icarus
Cassini 27
Spectroscopic classification of icy satellites of Saturn I: Identification of terrain units on Dione
DOI: 10.1016/j.icarus.2013.08.008 Bibcode: 2013Icar..226.1331S

Stephan, K.; Capaccioni, F.; Cerroni, P. +4 more

Dione is one of the largest and densest icy satellites of Saturn. Its surface shows a marked asymmetry between its leading and trailing hemispheres, the leading side being brighter than the trailing side, which shows regions mantled by a dark veneer whose origin is likely exogenic. In order to identify different terrain units we applied the Spectr…

2013 Icarus
Cassini 25