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Energy Deposition Processes in Titan's Upper Atmosphere and Its Induced Magnetosphere
DOI: 10.1007/978-1-4020-9215-2_16 Bibcode: 2010tfch.book..393S

Hartle, R. E.; Dandouras, Iannis; Coates, Andrew +4 more

Most of Titan's atmospheric organic and nitrogen chemistry, aerosol formation, and atmospheric loss are driven from external energy sources such as Solar UV, Saturn's magnetosphere, solar wind and galactic cosmic rays. The Solar UV tends to dominate the energy input at lower altitudes~1,200 km but which can extend down to ~400 km, while the plasma…

2010 Titan from Cassini-Huygens
Cassini 19
The Origin and Evolution of Titan
DOI: 10.1007/978-1-4020-9215-2_3 Bibcode: 2010tfch.book...35L

Choukroun, Mathieu; Lunine, Jonathan; Tobie, Gabriel +1 more

Titan was formed as a regular satellite in a disk that was the outgrowth of the formation of Saturn itself. Unlike the Jovian system, Titan is alone in terms of its size and mass, notart of a system gradational in density and hence rock abundance,erhaps reflecting a smaller disk and greater importance of stochastic events during satellite assembly…

2010 Titan from Cassini-Huygens
Cassini 18
Mass Loss Processes in Titan's Upper Atmosphere
DOI: 10.1007/978-1-4020-9215-2_15 Bibcode: 2010tfch.book..373J

Johnson, R. E.; Sittler, E. C.; Smith, H. T. +4 more

Although Titan's atmospheric column density is about ten times that of the Earth's, its measured 15N/14N ratio suggests that considerable escape has occurred or that Titan's original material had a ratio closer to that of cometary materials. A number of active escape processes have been proposed: thermal escape, chemical-induced escape, slow hydro…

2010 Titan from Cassini-Huygens
Cassini 15
Titan's Interior Structure
DOI: 10.1007/978-1-4020-9215-2_4 Bibcode: 2010tfch.book...61S

Sotin, Christophe; Rappaport, Nicole; Mitri, Giuseppe +2 more

The goal of this chapter is to give a description of Titan's interior that is consistent with the new constraints provided by the Cassini mission. As the Cassini mission proceeds into its first extended phase, the data obtained during the nominal mission suggest that Titan is at least partially differentiated. An ocean would be present some tens o…

2010 Titan from Cassini-Huygens
Cassini 14
Aerosols in Titan's Atmosphere
DOI: 10.1007/978-1-4020-9215-2_12 Bibcode: 2010tfch.book..297T

West, Robert A.; Tomasko, Martin G.

Aerosols in Titan's atmosphere play important roles in the transfer of solar and thermal radiation, in Titan's heat balance, in forcing atmospheric dynamics, and as a sink for photochemical reactions. In this chapter we briefly summarize the history of our knowledge of their distribution and optical properties before concentrating in greater detai…

2010 Titan from Cassini-Huygens
Cassini 13
Geology and Surface Processes on Titan
DOI: 10.1007/978-1-4020-9215-2_5 Bibcode: 2010tfch.book...75J

Sotin, Christophe; Tomasko, Martin G.; Keller, Horst Uwe +8 more

The surface of Titan has been revealed globally, if incompletely, by Cassini observations at infrared and radar wavelengths as well as locally by the instruments on the Huygens probe. Extended dune fields, lakes, mountainous terrain, dendritic erosion patterns and erosional remnants indicate dynamic surface processes. Valleys, small-scale gullies …

2010 Titan from Cassini-Huygens
Cassini 11
High-Altitude Production of Titan's Aerosols
DOI: 10.1007/978-1-4020-9215-2_8 Bibcode: 2010tfch.book..201W

Young, D. T.; Lunine, J. I.; Westlake, J. +3 more

Measurements with the Cassini Ion and Neutral Mass Spectrometer (INMS) and two Cassini Plasma Spectrometer (CAPS) sensors, the Ion beam Spectrometer (IBS) and the Electron Spectrometer (ELS), have revealed the presence of a significant population of heavy hydrocarbon and nitrile species well above the homopause, with masses as large as several tho…

2010 Titan from Cassini-Huygens
Cassini 7
Composition of Titan's Surface
DOI: 10.1007/978-1-4020-9215-2_6 Bibcode: 2010tfch.book..141S

Barnes, J. W.; Brown, R. H.; Clark, R. N. +5 more

The Huygens Probe returned the first in situ data on Titan's surface composition in January 2005. Although Huygens landed on a dry plain, the Gas Chromatograph Mass Spectrometer (GCMS) showed evidence of methane moisture in the near subsurface suggesting methane precipitation at some time in the past. Heavier organic molecules were not found to be…

2010 Titan from Cassini-Huygens
Cassini 6
Seasonal Change on Titan
DOI: 10.1007/978-1-4020-9215-2_14 Bibcode: 2010tfch.book..353L

Flasar, F. Michael; Lorenz, Ralph D.; Brown, Michael E.

Titan displays seasonal changes in the distribution of gas and hazes in its atmosphere, in the character of its methane clouds, and in its temperatures and winds. While Cassini has observed some of these changes in detail, some are observable from Earth, and the period of most rapid change may be just about to begin in the years after equinox.

2010 Titan from Cassini-Huygens
Cassini 5
Mapping Products of Titan's Surface
DOI: 10.1007/978-1-4020-9215-2_19 Bibcode: 2010tfch.book..489S

Barnes, Jason W.; Le Mouélic, Stéphane; Karkoschka, Erich +9 more

Remote sensing instruments aboard the Cassini spacecraft have been observed the surface of Titan globally in the infrared and radar wavelength ranges as well as locally by the Huygens instruments revealing a wealth of new morphological features indicating a geologically active surface. We present a summary of mapping products of Titan's surface de…

2010 Titan from Cassini-Huygens
Cassini 4