Ion Neutral Mass Spectrometer results from the first flyby of Titan

被引:366
作者
Waite, JH [1 ]
Niemann, H
Yelle, RV
Kasprzak, WT
Cravens, TE
Luhmann, JG
McNutt, RL
Ip, WH
Gell, D
De La Haye, V
Müller-Wordag, I
Magee, B
Borggren, N
Ledvina, S
Fletcher, G
Walter, E
Miller, R
Scherer, S
Thorpe, R
Xu, J
Block, B
Arnett, K
机构
[1] Univ Michigan, Dept Atmospher Ocean & Space Sci, Ann Arbor, MI 48109 USA
[2] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[3] Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA
[4] Univ Kansas, Dept Phys & Astron, Lawrence, KS 66045 USA
[5] Univ Calif Berkeley, Space Sci Lab, Berkeley, CA 94720 USA
[6] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD 20723 USA
[7] Natl Cent Univ, Inst Astron, Chungli 32054, Taiwan
[8] Univ London Imperial Coll Sci Technol & Med, Space & Atmospher Phys Grp, London SW7 2BW, England
[9] SW Res Inst, San Antonio, TX 78228 USA
关键词
D O I
10.1126/science.1110652
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The Cassini Ion Neutral Mass Spectrometer (INMS) has obtained the first in situ composition measurements of the neutral densities of molecular nitrogen, methane, molecular hydrogen, argon, and a host of stable carbon-nitrile compounds in Titan's upper atmosphere. INMS in situ mass spectrometry has also provided evidence for atmospheric waves in the upper atmosphere and the first direct measurements of isotopes of nitrogen, carbon, and argon, which reveal interesting clues about the evolution of the atmosphere. The bulk composition and thermal structure of the moon's upper atmosphere do not appear to have changed considerably since the Voyager 1 flyby.
引用
收藏
页码:982 / 986
页数:5
相关论文
共 28 条
[1]   EVOLUTION OF A NITROGEN ATMOSPHERE ON TITAN [J].
ATREYA, SK ;
DONAHUE, TM ;
KUHN, WR .
SCIENCE, 1978, 201 (4356) :611-613
[2]   TITANS ATMOSPHERE FROM VOYAGER INFRARED OBSERVATIONS .1. THE GAS-COMPOSITION OF TITANS EQUATORIAL REGION [J].
COUSTENIS, A ;
BEZARD, B ;
GAUTIER, D .
ICARUS, 1989, 80 (01) :54-76
[3]   Photochemical sources of non-thermal neutrals for the exosphere of Titan [J].
Cravens, TE ;
Keller, CN ;
Ray, B .
PLANETARY AND SPACE SCIENCE, 1997, 45 (08) :889-896
[4]  
FEGLEY B, 1995, GLOBAL EARTH PHYS HD, P320, DOI DOI 10.1029/RF001P0320
[5]   Titan's atmospheric temperatures, winds, and composition [J].
Flasar, FM ;
Achterberg, RK ;
Conrath, BJ ;
Gierasch, PJ ;
Kunde, VG ;
Nixon, CA ;
Bjoraker, GL ;
Jennings, DE ;
Romani, PN ;
Simon-Miller, AA ;
Bézard, B ;
Coustenis, A ;
Irwin, PGJ ;
Teanby, NA ;
Brasunas, J ;
Pearl, JC ;
Segura, ME ;
Carlson, RC ;
Mamoutkine, A ;
Schinder, PJ ;
Barucci, A ;
Courtin, R ;
Fouchet, T ;
Gautier, D ;
Lellouch, E ;
Marten, A ;
Prangé, R ;
Vinatier, S ;
Strobel, DF ;
Calcutt, SB ;
Read, PL ;
Taylor, FW ;
Bowles, N ;
Samuelson, RE ;
Orton, GS ;
Spilker, LJ ;
Owen, TC ;
Spencer, JR ;
Showalter, MR ;
Ferrari, C ;
Abbas, MM ;
Raulin, F ;
Edgington, S ;
Ade, P ;
Wishnow, EH .
SCIENCE, 2005, 308 (5724) :975-978
[6]   Formation and composition of planetesimals - Trapping volatiles by clathration [J].
Gautier, D ;
Hersant, F .
SPACE SCIENCE REVIEWS, 2005, 116 (1-2) :25-52
[7]   Submillimeter observations of Titan:: Global measures of stratospheric temperature, CO, HCN, HC3N, and the isotopic ratios 12C/13C and 14N/15N [J].
Gurwell, MA .
ASTROPHYSICAL JOURNAL, 2004, 616 (01) :L7-L10
[8]   Millimeter and submillimeter heterodyne observations of titan, retrieval of the vertical profile of HCN and the C-12/C-13 ratio [J].
Hidayat, T ;
Marten, A ;
Bezard, B ;
Gautier, D ;
Owen, T ;
Matthews, HE ;
Paubert, G .
ICARUS, 1997, 126 (01) :170-182
[9]  
JOHNS TF, 1957, ATOMIC ENERGY RES ES
[10]  
Kallenbach R, 1998, ASTROPHYS J, V507, pL185, DOI 10.1086/311702