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Ion Neutral Mass Spectrometer Results from the First Flyby of Titan
J. Hunter Waite, Jr.,1Hasso Niemann,2Roger V. Yelle,3Wayne T. Kasprzak,2Thomas E. Cravens,4Janet G. Luhmann,5Ralph L. McNutt,6Wing-Huen Ip,7David Gell,1Virginie De La Haye,1Ingo Müller-Wordag,8Brian Magee,1Nathan Borggren,3Steve Ledvina,5Greg Fletcher,1Erin Walter,1Ryan Miller,1Stefan Scherer,1Rob Thorpe,9Jing Xu,1Bruce Block,1Ken Arnett1
The Cassini Ion Neutral Mass Spectrometer (INMS) has obtainedthe first in situ composition measurements of the neutral densitiesof molecular nitrogen, methane, molecular hydrogen, argon, anda host of stable carbon-nitrile compounds in Titan's upper atmosphere.INMS in situ mass spectrometry has also provided evidence foratmospheric waves in the upper atmosphere and the first directmeasurements of isotopes of nitrogen, carbon, and argon, whichreveal interesting clues about the evolution of the atmosphere.The bulk composition and thermal structure of the moon's upperatmosphere do not appear to have changed considerably sincethe Voyager 1 flyby.
1 Department of Atmospheric, Oceanic, and Space Sciences, University of Michigan, Ann Arbor, MI 481092143, USA. 2 NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA. 3 Lunar and Planetary Laboratory, University of Arizona, 1629 East University Boulevard, Tucson, AZ 857210092, USA. 4 Department of Physics and Astronomy, University of Kansas, Lawrence, KS 66045, USA. 5 Space Sciences Laboratory, University of California, Berkeley, CA 94720, USA. 6 Applied Physics Laboratory, Johns Hopkins University, Laurel, MD 20723, USA. 7 Institute of Astronomy, National Central University, Chung-Li 32054, Taiwan. 8 Space and Atmospheric Physics Group, Imperial College, London SW7 2BW, UK. 9 Southwest Research Institute, Post Office Drawer 28510, San Antonio, TX 782280510, USA.
Titan's exosphere and its interaction with Saturn's magnetosphere.
I. Dandouras, P. Garnier, D. G Mitchell, E. C Roelof, P. C Brandt, N. Krupp, and S. M Krimigis (2009)
Phil Trans R Soc A
367, 743-752
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Sputtering and heating of Titan's upper atmosphere.
The Process of Tholin Formation in Titan's Upper Atmosphere.
J. H. Waite Jr., D. T. Young, T. E. Cravens, A. J. Coates, F. J. Crary, B. Magee, and J. Westlake (2007)
Science
316, 870-875
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Inaugural Article: Organic haze on Titan and the early Earth.
M. G. Trainer, A. A. Pavlov, H. L. DeWitt, J. L. Jimenez, C. P. McKay, O. B. Toon, and M. A. Tolbert (2006)
PNAS
103, 18035-18042
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