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Discovery of heavy negative ions in Titan's ionosphere
DOI: 10.1029/2007GL030978 Bibcode: 2007GeoRL..3422103C

Lewis, G. R.; Coates, A. J.; Sittler, E. C. +3 more

Titan's ionosphere contains a rich positive ion population including organic molecules. Here, using CAPS electron spectrometer data from sixteen Titan encounters, we reveal the existence of negative ions. These ions, with densities up to ~100 cm-3, are in mass groups of 10-30, 30-50, 50-80, 80-110, 110-200 and 200+ amu/charge. During on…

2007 Geophysical Research Letters
Cassini 347
Pressurized oceans and the eruption of liquid water on Europa and Enceladus
DOI: 10.1029/2007GL029297 Bibcode: 2007GeoRL..34.7202M

Manga, M.; Wang, C. -Y.

It is difficult for liquid water to erupt onto the surface of icy satellites, such as Europa and Enceladus, because liquid water is more dense than ice. If the ice shell thickens, the volume expansion of ice upon freezing increases pressure in the subsurface ocean. The excess pressure is determined by a balance between compression of ocean water a…

2007 Geophysical Research Letters
Cassini 113
A Saturnian longitude system based on a variable kilometric radiation period
DOI: 10.1029/2006GL028336 Bibcode: 2007GeoRL..34.2201K

Gurnett, D. A.; Kurth, W. S.; Averkamp, T. F. +2 more

This paper describes a longitude system for Saturn which is locked to the period of Saturn kilometric radiation. Because the apparent radio emission period varies with time, the period used in the system is allowed to vary. The resulting system results in the 'diurnal' peak of the radio emission occurring when the subsolar longitude is 100°, as wa…

2007 Geophysical Research Letters
Cassini 106
Strong rapid dipolarizations in Saturn's magnetotail: In situ evidence of reconnection
DOI: 10.1029/2007GL029764 Bibcode: 2007GeoRL..3411203J

Russell, C. T.; Dougherty, M. K.; Jackman, C. M. +3 more

The oppositely directed magnetic field in the kronian magnetic tail is expected eventually to reconnect across the current sheet, allowing plasma to escape in an anti-solar direction down the tail. This reconnection process accelerates ions and electrons both toward and away from the planet, allowing the magnetotail to relax to a more dipolar conf…

2007 Geophysical Research Letters
Cassini 84
Titan's young surface: Initial impact crater survey by Cassini RADAR and model comparison
DOI: 10.1029/2006GL028971 Bibcode: 2007GeoRL..34.7204L

Lorenz, R. D.; Anderson, Y. Z.; Lunine, J. I. +9 more

Cassini's Radar instrument has mapped over 10% of Titan's surface through the T18 flyby in August 2006 and has detected remarkably few impact craters. Three impact craters have been conclusively identified and named, and a handful of unconfirmed candidate impact structures are documented. These results indicate that the overall crater density is a…

2007 Geophysical Research Letters
Cassini 78
Ring current at Saturn: Energetic particle pressure in Saturn's equatorial magnetosphere measured with Cassini/MIMI
DOI: 10.1029/2006GL029223 Bibcode: 2007GeoRL..34.9102S

Krupp, N.; Krimigis, S. M.; Mitchell, D. G. +5 more

The Magnetospheric Imaging Instrument (MIMI) on the Cassini spacecraft provides measurements of the energetic ion population within the magnetosphere of Saturn. Energetic ion directional intensities, energy spectra and ion composition, are measured by the Charge Energy Mass Spectrometer (CHEMS) over the range ~3 to 236 keV per charge and by the Lo…

2007 Geophysical Research Letters
Cassini 74
Ionospheric electrons in Titan's tail: Plasma structure during the Cassini T9 encounter
DOI: 10.1029/2007GL030919 Bibcode: 2007GeoRL..3424S05C

Coates, A. J.; Hartle, R. E.; Sittler, E. C. +6 more

We present results from the CAPS electron spectrometer obtained during the downstream flyby of Titan on 26 December 2005, which occurred during a period of enhanced plasma pressure inside the magnetosphere. The electron data show an unusual split signature with two principal intervals of interest outside the nominal corotation wake. Interval 1 sho…

2007 Geophysical Research Letters
Cassini 69
Convection in Enceladus' ice shell: Conditions for initiation
DOI: 10.1029/2006GL028799 Bibcode: 2007GeoRL..34.9202B

McKinnon, William B.; Barr, Amy C.

Observations of Enceladus by the Cassini spacecraft indicate that this tiny Saturnian moon is geologically active, with plumes of water vapor and ice particles erupting from its southern polar region. This activity suggests that tidal dissipation has become spatially localized, perhaps due to a compositional, rheological, and/or thermal anomaly in…

2007 Geophysical Research Letters
Cassini 69
Role of photoionization in the formation of complex organic molecules in Titan's upper atmosphere
DOI: 10.1029/2006GL028317 Bibcode: 2007GeoRL..34.2204I

Imanaka, Hiroshi; Smith, Mark A.

Recent observations by the Cassini Orbiter suggest that complex organic chemistry occurs in the upper atmosphere of Titan. To understand the role of EUV-VUV light in the complex organic chemistry of Titan's upper atmosphere, we investigate the formation of gaseous species from a N2/CH4 gas mixture as a function of irradiation…

2007 Geophysical Research Letters
Cassini 57
Mass of Saturn's magnetodisc: Cassini observations
DOI: 10.1029/2006GL028921 Bibcode: 2007GeoRL..34.9108A

André, N.; Coates, A. J.; Russell, C. T. +5 more

Saturn's ring current was observed by Pioneer 11 and the two Voyager spacecraft to extend 8-16 R S in the equatorial plane and appeared to be driven by stress balance with the centrifugal force. We present Cassini observations that show thin current sheets on the dawn flank of Saturn's magnetosphere, symptomatic of the formation of a …

2007 Geophysical Research Letters
Cassini 51