Search Publications

Analysis of Saturn’s thermal emission at 2.2-cm wavelength: Spatial distribution of ammonia vapor
DOI: 10.1016/j.icarus.2013.06.017 Bibcode: 2013Icar..226..641L

Janssen, M. A.; Allison, M.; Ingersoll, A. P. +3 more

This work focuses on determining the latitudinal structure of ammonia vapor in Saturn’s cloud layer near 1.5 bars using the brightness temperature maps derived from the Cassini RADAR (Elachi et al. [2004], Space Sci. Rev. 115, 71-110) instrument, which works in a passive mode to measure thermal emission from Saturn at 2.2-cm wavelength. We perform…

2013 Icarus
Cassini 21
Synergistic observations of Io’s atmosphere in 2010 from HST-COS in the mid-ultraviolet and IRTF-TEXES in the mid-infrared
DOI: 10.1016/j.icarus.2013.06.010 Bibcode: 2013Icar..226..604T

Tsang, Constantine C. C.; Spencer, John R.; Jessup, Kandis Lea

We report on mid-UV spectroscopy of Io’s SO2 atmosphere from the Cosmic Origins Spectrograph (COS) on the Hubble Space Telescope (HST), and compare to contemporaneous ground-based mid-infrared spectroscopy of the atmosphere. Our motivation is to evaluate the consistency of atmospheric parameters derived by different observational techni…

2013 Icarus
eHST 20
Auroral electron precipitation and flux tube erosion in Titan’s upper atmosphere
DOI: 10.1016/j.icarus.2013.05.021 Bibcode: 2013Icar..226..186S

Coates, A. J.; Jones, G. H.; Wellbrock, A. +4 more

Cassini dasta shows that Titan’s atmosphere strongly depletes the electron content in Saturn’s flux tubes, producing features known as electron bite-outs, which indicate that the flux of auroral electrons decreases over time. To understand this process we have developed a time-dependent two-stream model, which uses field line geometries and drift …

2013 Icarus
Cassini 19
The behavior of spokes in Saturn's B ring
DOI: 10.1016/j.icarus.2013.02.011 Bibcode: 2013Icar..225..446M

Porco, C. C.; Spitale, J. N.; Mitchell, C. J. +1 more

We present the first results from Cassini ISS observations aimed at determining both the short-term and long-term behavior of the spokes in Saturn's B ring. We have observed multiple spokes which appear between images where there was not a spoke before. The radial termini of these new spokes expand radially at ∼0.5 km/s in both the inward and outw…

2013 Icarus
Cassini 19
Local spectrophotometric properties of pyroclastic deposits at the Lavoisier lunar crater
DOI: 10.1016/j.icarus.2013.03.004 Bibcode: 2013Icar..225....1S

Besse, S.; Josset, J. -L.; Haruyama, J. +5 more

We present a study of the Lavoisier lunar crater combining photometric data from the AMIE camera (SMART-1 mission) and hyperspectral data from the Moon Mineralogy Mapper M3 (Chandrayaan-1 mission), with a special emphasis on the pyroclastic deposits considered to be present on the crater floor. The photometric parameters are in agreemen…

2013 Icarus
Chandrayaan-1 SMART-1 18
Does ice float in Titan’s lakes and seas?
DOI: 10.1016/j.icarus.2012.11.028 Bibcode: 2013Icar..223..628H

Lunine, Jonathan I.; Hofgartner, Jason D.

We model Titan’s lakes and seas as methane-ethane-nitrogen systems and model the buoyancy of solids in these systems assuming thermodynamic equilibrium. We find that ice will float in methane-rich lakes for all temperatures below the freezing point of pure methane and that ice will also float in ethane-rich seas provided the ice has an air porosit…

2013 Icarus
Cassini 18
Venus nitric oxide nightglow mapping from SPICAV nadir observations
DOI: 10.1016/j.icarus.2013.05.031 Bibcode: 2013Icar..226..428S

Bertaux, J. -L.; Gérard, J. -C.; Stiepen, A. +2 more

Nitric oxide δ (190-240 nm) and γ (255-270 nm) bands have been observed on the Venus nightside with Venus Express SPICAV instrument operated in the nadir mode. These ultraviolet emissions arise from the de-excitation of NO molecules created by radiative recombination of O(3P) and N(4S) atoms. These atoms are produced on the d…

2013 Icarus
VenusExpress 18
Saturn’s ring temperatures at equinox
DOI: 10.1016/j.icarus.2013.06.002 Bibcode: 2013Icar..226..316S

Spilker, Linda; Ferrari, Cecile; Morishima, Ryuji

Modeling the thermal emission of Saturn’s rings is challenging due to the numerous heating sources as well as the structural properties of the disk and of the particles that are closely related. At equinox, however, rings are externally heated by Saturn alone and the problem is somewhat simplified. We test the abilities of our current models to re…

2013 Icarus
Cassini 17
Hubble observations of Jupiter’s north-south conjugate ultraviolet aurora
DOI: 10.1016/j.icarus.2013.08.017 Bibcode: 2013Icar..226.1559G

Bonfond, B.; Clarke, J. T.; Gérard, J. -C. +2 more

Comparisons of the northern and southern far ultraviolet (UV) auroral emissions of Jupiter from the Hubble Space Telescope (HST) or any other ultraviolet imager have mostly been made so far on a statistical basis or were not obtained with high sensitivity and resolution. Such observations are important to discriminate between different mechanisms …

2013 Icarus
eHST 17
The smallest particles in Saturn’s A and C Rings
DOI: 10.1016/j.icarus.2013.08.015 Bibcode: 2013Icar..226.1225H

Nicholson, Philip D.; Hedman, Matthew M.; Harbison, Rebecca A.

Radio occultations of Saturn’s main rings by spacecraft suggest a power law particle size-distribution down to sizes of the order of 1 cm (Marouf, E.A., Tyler, G.L., Zebker, H.A., Simpson, R.A., Eshleman, V.R. [1983]. Icarus 54, 189-211; Zebker, H.A., Marouf, E.A., Tyler, G.L. [1985]. Icarus 64, 531-548.). The lack of optical depth variations betw…

2013 Icarus
Cassini 16