Search Publications

Negative ion chemistry in Titan's upper atmosphere
DOI: 10.1016/j.pss.2009.04.004 Bibcode: 2009P&SS...57.1558V

Lewis, G. R.; Coates, A. J.; Wahlund, J. -E. +5 more

The Electron Spectrometer (ELS), one of the sensors making up the Cassini Plasma Spectrometer (CAPS) revealed the existence of numerous negative ions in Titan's upper atmosphere. The observations at closest approach (∼1000 km) show evidence for negatively charged ions up to ∼10,000 amu/q, as well as two distinct peaks at 22±4 and 44±8 amu/q, and m…

2009 Planetary and Space Science
Cassini 201
INMS-derived composition of Titan's upper atmosphere: Analysis methods and model comparison
DOI: 10.1016/j.pss.2009.06.016 Bibcode: 2009P&SS...57.1895M

Mandt, Kathleen E.; Waite, J. Hunter; Magee, Brian A. +3 more

The Cassini Ion and Neutral Mass Spectrometer (INMS) has recorded full altitude profile data from 20 low-altitude Titan encounters during the nominal mission (July 2004-2008). These encounters were TA, T5, T16, T18, T19, T21, T23, T25, T26, T28, T29, T30, T32, T36, T37, T39, T40, T41, T42, and T43. In this work we present an analysis of the data o…

2009 Planetary and Space Science
Cassini 143
Recurrent energization of plasma in the midnight-to-dawn quadrant of Saturn's magnetosphere, and its relationship to auroral UV and radio emissions
DOI: 10.1016/j.pss.2009.04.002 Bibcode: 2009P&SS...57.1732M

Gurnett, D. A.; Dougherty, M. K.; Krimigis, S. M. +11 more

We demonstrate that under some magnetospheric conditions protons and oxygen ions are accelerated once per Saturn magnetosphere rotation, at a preferred local time between midnight and dawn. Although enhancements in energetic neutral atom (ENA) emission may in general occur at any local time and at any time in a Saturn rotation, those enhancements …

2009 Planetary and Space Science
Cassini eHST 125
Detection of dusty plasma near the E-ring of Saturn
DOI: 10.1016/j.pss.2009.03.011 Bibcode: 2009P&SS...57.1795W

Gurnett, D. A.; Hospodarsky, G. B.; Kurth, W. S. +12 more

We present several independent in-situ measurements, which provide evidence that charged dust in the E-ring interacts collectively with the dense surrounding plasma disk of Saturn, i.e., form a system of dust-plasma interaction. The results are based on data sampled by the Radio and Plasma Wave Science (RPWS) investigation onboard Cassini, which a…

2009 Planetary and Space Science
Cassini 114
Heavy ions, temperatures and winds in Titan's ionosphere: Combined Cassini CAPS and INMS observations
DOI: 10.1016/j.pss.2009.09.006 Bibcode: 2009P&SS...57.1847C

Young, D. T.; Waite, J. H.; Magee, B. A. +3 more

Multiple Titan encounters by the Cassini spacecraft have shown that ion chemistry in Titan's upper atmosphere is much more complex than previously thought. As well as showing a great variety of species present below 100 amu, they also include the detection of negative ions and of large abundances of ions above 100 amu. Here, we use data from two C…

2009 Planetary and Space Science
Cassini 97
On the ionospheric structure of Titan
DOI: 10.1016/j.pss.2009.04.012 Bibcode: 2009P&SS...57.1821A

Garnier, P.; Wahlund, J. -E.; Ågren, K. +4 more

In this study we present data from 17 Titan flybys showing that solar photons are the main ionisation source of Titan's dayside atmosphere. This is the first comprehensive study of Solar Zenith Angle (SZA) dependence of the electron number density and electron temperature at the ionospheric peak. The results show on average four times more plasma …

2009 Planetary and Space Science
Cassini 93
Heavy negative ions in Titan's ionosphere: Altitude and latitude dependence
DOI: 10.1016/j.pss.2009.05.009 Bibcode: 2009P&SS...57.1866C

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

One of the unexpected results of the Cassini mission was the discovery of negative ions at altitudes between 950 and 1400 km in Titan's ionosphere with masses up to 10,000 amu/q [Coates, A.J., Crary, F.J., Lewis, G.R., Young, D.T., Waite Jr., J.H., Sittler Jr., E.C., 2007. Discovery of heavy negative ions in Titan's ionosphere. Geophys. Res. Lett.…

2009 Planetary and Space Science
Cassini 87
Saturn's north polar cyclone and hexagon at depth revealed by Cassini/VIMS
DOI: 10.1016/j.pss.2009.06.026 Bibcode: 2009P&SS...57.1671B

Nicholson, Philip D.; Fletcher, Leigh N.; Baines, Kevin H. +6 more

A high-speed cyclonic vortex centered on the north pole of Saturn has been revealed by the visual-infrared mapping spectrometer (VIMS) onboard the Cassini-Huygens Orbiter, thus showing that the tropospheres of both poles of Saturn are occupied by cyclonic vortices with winds exceeding 135 m/s. High-spatial-resolution (~200 km per pixel) images acq…

2009 Planetary and Space Science
Cassini 78
Plasma in Saturn's nightside magnetosphere and the implications for global circulation
DOI: 10.1016/j.pss.2009.03.003 Bibcode: 2009P&SS...57.1714M

Coates, A. J.; Dougherty, M. K.; Thomsen, M. F. +8 more

We present a bulk ion flow map from the nightside, equatorial region of Saturn's magnetosphere derived from the Cassini CAPS ion mass spectrometer data. The map clearly demonstrates the dominance of corotation flow over radial flow and suggests that the flux tubes sampled are still closed and attached to the planet up to distances of 50 RS

2009 Planetary and Space Science
Cassini 76
Isotopic evolution of the major constituents of Titan's atmosphere based on Cassini data
DOI: 10.1016/j.pss.2009.06.005 Bibcode: 2009P&SS...57.1917M

Mousis, Olivier; Mandt, Kathleen E.; Waite, J. Hunter +5 more

Using Cassini ion neutral mass spectrometer stable isotope observations, we have developed a comprehensive method for modeling the time-evolution of the stable isotopic ratios in Titan's major constituents, N 2, CH 4 and H 2. Our model provides constraints on the initial 14N/ 15N ratio in N

2009 Planetary and Space Science
Cassini 65