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Latitudinal variations of HCN, HC 3N, and C 2N 2 in Titan's stratosphere derived from Cassini CIRS data
DOI: 10.1016/j.icarus.2005.11.008 Bibcode: 2006Icar..181..243T

Fletcher, L.; Irwin, P. G. J.; Teanby, N. A. +9 more

Mid- and far-infrared spectra from the Composite InfraRed Spectrometer (CIRS) have been used to determine volume mixing ratios of nitriles in Titan's atmosphere. HCN, HC 3N, C 2H 2, and temperature were derived from 2.5 cm -1 spectral resolution mid-IR mapping sequences taken during three flybys, which p…

2006 Icarus
Cassini 103
Jupiter's atmospheric temperatures: From Voyager IRIS to Cassini CIRS
DOI: 10.1016/j.icarus.2005.07.019 Bibcode: 2006Icar..180...98S

Achterberg, Richard K.; Flasar, F. Michael; Simon-Miller, Amy A. +4 more

Retrievals performed on Cassini Composite Infrared Spectrometer data obtained during the distant Jupiter flyby in 2000/2001 have been used to generate global temperature maps of the planet in the troposphere and stratosphere, but to higher latitudes than were shown previously by Flasar et al. [Flasar, F.M., 39 colleagues, 2004a. Nature 427, 132-13…

2006 Icarus
Cassini 100
Interaction between eddies and mean flow in Jupiter's atmosphere: Analysis of Cassini imaging data
DOI: 10.1016/j.icarus.2006.08.007 Bibcode: 2006Icar..185..430S

Ingersoll, Andrew P.; Del Genio, Anthony D.; Vasavada, Ashwin +2 more

Beebe et al. [Beebe, R.F., et al., 1980. Geophys. Res. Lett. 17, 1-4] and Ingersoll et al. [Ingersoll, A.P., et al., 1981. J. Geophys. Res. 86, 8733-8743] used images from Voyagers 1 and 2 to analyze the interaction between zonal winds and eddies in Jupiter's atmosphere. They reported a high positive correlation between Jupiter's eddy momentum flu…

2006 Icarus
Cassini 98
Production, ionization and redistribution of O 2 in Saturn's ring atmosphere
DOI: 10.1016/j.icarus.2005.08.021 Bibcode: 2006Icar..180..393J

Luhmann, J. G.; Tokar, R. L.; Johnson, R. E. +10 more

Molecular oxygen produced by the decomposition of icy surfaces is ubiquitous in Saturn's magnetosphere. A model is described for the toroidal O 2 atmosphere indicated by the detection of O2+ and O + over the main rings. The O 2 ring atmosphere is produced primarily by UV photon-induced decomposition of ice on the s…

2006 Icarus
Cassini 87
The vertical structure of Titan's upper atmosphere from Cassini Ion Neutral Mass Spectrometer measurements
DOI: 10.1016/j.icarus.2005.10.029 Bibcode: 2006Icar..182..567Y

Waite, J. H.; Kasprzak, W. T.; Müller-Wodarg, I. +4 more

Data acquired by the Ion Neutral Mass Spectrometer (INMS) on the Cassini spacecraft during its close encounter with Titan on 26 October 2004 reveal the structure of its upper atmosphere. Altitude profiles of N 2, CH 4, and H 2, inferred from INMS measurements, determine the temperature, vertical mixing rate, and es…

2006 Icarus
Cassini 83
A large cloud outburst at Titan's south pole
DOI: 10.1016/j.icarus.2005.12.021 Bibcode: 2006Icar..182..224S

Brown, Michael E.; Bouchez, Antonin H.; Roe, Henry G. +1 more

Images of Titan acquired over five nights in October 2004 using the adaptive optics system at the Keck Observatory show dramatic increases in tropospheric cloud activity at the south pole compared with all other images of Titan clouds to date. During this time, Titan's south polar clouds brightened to more than 18 times their typical values. The C…

2006 Icarus
Cassini 81
Reflectance spectra and chemical structure of Titan's tholins: Application to the analysis of Cassini Huygens observations
DOI: 10.1016/j.icarus.2006.06.004 Bibcode: 2006Icar..185..301B

Quirico, E.; Schmitt, B.; Coll, P. +7 more

Titan's tholins are used as analogs of Titan's aerosols and N-rich organic solids present on many icy surfaces. However, it is not clear whether or not they are relevant analogs, and which kind of tholins should be used among a wide set available in literature. This paper presents reflectance spectral data of two tholins selected as end-members of…

2006 Icarus
Cassini 77
Cassini RADAR observations of Enceladus, Tethys, Dione, Rhea, Iapetus, Hyperion, and Phoebe
DOI: 10.1016/j.icarus.2006.02.019 Bibcode: 2006Icar..183..479O

Black, Gregory J.; Lorenz, Ralph D.; Hensley, Scott +17 more

Cassini 2.2-cm radar and radiometric observations of seven of Saturn's icy satellites yield properties that apparently are dominated by subsurface volume scattering and are similar to those of the icy Galilean satellites. Average radar albedos decrease in the order Enceladus/Tethys, Hyperion, Rhea, Dione, Iapetus, and Phoebe. This sequence most li…

2006 Icarus
Cassini 76
Dissipation of Titan's south polar clouds
DOI: 10.1016/j.icarus.2006.05.025 Bibcode: 2006Icar..184..517S

Brown, Michael E.; Trujillo, Chadwick A.; Bouchez, Antonin H. +2 more

Nearly all adaptive optics images of Titan taken between December 2001 and November 2004 showed tropospheric clouds located within 30° of the south pole. We report here on a dissipation of Titan's south polar clouds observed in twenty-nine Keck and Gemini images taken between December 2004 and April 2005. The near complete lack of south polar clou…

2006 Icarus
Cassini 72
A global circulation model of Saturn's thermosphere
DOI: 10.1016/j.icarus.2005.09.002 Bibcode: 2006Icar..180..147M

Yelle, R. V.; Müller-Wodarg, I. C. F.; Aylward, A. D. +1 more

We present the first 3-dimensional self-consistent calculations of the response of Saturn's global thermosphere to different sources of external heating, giving local time and latitudinal changes of temperatures, winds and composition at equinox and solstice. Our calculations confirm the well-known finding that solar EUV heating alone is insuffici…

2006 Icarus
Cassini 65