No oceans on Titan from the absence of a near-infrared specular reflection

被引:49
作者
West, RA
Brown, ME
Salinas, SV
Bouchez, AH
Roe, HG
机构
[1] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[2] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
[3] Natl Univ Singapore, Ctr Remote Imaging Sensing & Proc, Singapore 119260, Singapore
[4] WM Keck Observ, Kamuela, HI 96743 USA
关键词
D O I
10.1038/nature03824
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
With its substantial atmosphere of nitrogen, hydrocarbons and nitriles, Saturn's moon Titan is a unique planetary satellite. Photochemical processing of the gaseous constituents produces an extended haze that obscures the surface. Soon after the Voyager fly-bys in 1980 and 1981 photochemical models(1-3) led to the conclusion that there should be enough liquid methane/ethane/ nitrogen to cover the surface to a depth of several hundred metres. Recent Earth-based radar echoes imply that surface liquid may be present at a significant fraction of the locations sampled(4). Here we present ground-based observations ( at near-infrared wavelengths) and calculations showing that there is no evidence thus far for surface liquid(5). Combined with the specular signatures from radar observations, we infer mechanisms that produce very flat solid surfaces, involving a substance that was liquid in the past but is not in liquid form at the locations we studied.
引用
收藏
页码:670 / 672
页数:3
相关论文
共 17 条
[1]  
BOUCHEZ AH, 2004, B AM ASTRON SOC, V36, P1696
[2]   Direct detection of variable tropospheric clouds near Titan's south pole [J].
Brown, ME ;
Bouchez, AH ;
Griffith, CA .
NATURE, 2002, 420 (6917) :795-797
[3]   The Cassini visual and infrared mapping spectrometer (VIMS) investigation [J].
Brown, RH ;
Baines, KH ;
Bellucci, G ;
Bibring, JP ;
Buratti, BJ ;
Capaccioni, F ;
Cerroni, P ;
Clark, RN ;
Coradini, A ;
Cruikshank, DP ;
Drossart, P ;
Formisano, V ;
Jaumann, R ;
Langevin, Y ;
Matson, DL ;
Mccord, TB ;
Mennella, V ;
Miller, E ;
Nelson, RM ;
Nicholson, PD ;
Sicardy, B ;
Sotin, C .
SPACE SCIENCE REVIEWS, 2004, 115 (1-4) :111-168
[4]   Radar evidence for liquid surfaces on Titan [J].
Campbell, DB ;
Black, GJ ;
Carter, LM ;
Ostro, SJ .
SCIENCE, 2003, 302 (5644) :431-434
[5]   FOURIER-SERIES EXPANSION OF THE TRANSFER EQUATION IN THE ATMOSPHERE OCEAN SYSTEM [J].
DEUZE, JL ;
HERMAN, M ;
SANTER, R .
JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER, 1989, 41 (06) :483-494
[6]   A NEW POLARIZED ATMOSPHERIC RADIATIVE-TRANSFER MODEL [J].
EVANS, KF ;
STEPHENS, GL .
JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER, 1991, 46 (05) :413-423
[7]   OCEANS ON TITAN [J].
FLASAR, FM .
SCIENCE, 1983, 221 (4605) :55-57
[8]  
GIBBARD SG, 2004, GEOPHYS RES LETT, V32, DOI UNSP L17S02
[9]   Inverse radiation modeling of Titan's atmosphere to assimilate solar aureole imager data of the Huygens probe [J].
Grieger, B ;
Lemmon, MT ;
Markiewicz, WJ ;
Keller, HU .
PLANETARY AND SPACE SCIENCE, 2003, 51 (02) :147-158
[10]   OPTICAL-CONSTANTS OF ORGANIC THOLINS PRODUCED IN A SIMULATED TITANIAN ATMOSPHERE - FROM SOFT-X-RAY TO MICROWAVE-FREQUENCIES [J].
KHARE, BN ;
SAGAN, C ;
ARAKAWA, ET ;
SUITS, F ;
CALLCOTT, TA ;
WILLIAMS, MW .
ICARUS, 1984, 60 (01) :127-137