THE THERMAL STRUCTURE OF TRITON ATMOSPHERE - RESULTS FROM THE 1993 AND 1995 OCCULTATIONS

Citation
Cb. Olkin et al., THE THERMAL STRUCTURE OF TRITON ATMOSPHERE - RESULTS FROM THE 1993 AND 1995 OCCULTATIONS, Icarus, 129(1), 1997, pp. 178-201
Citations number
44
Categorie Soggetti
Astronomy & Astrophysics
Journal title
IcarusACNP
ISSN journal
00191035
Volume
129
Issue
1
Year of publication
1997
Pages
178 - 201
Database
ISI
SICI code
0019-1035(1997)129:1<178:TTSOTA>2.0.ZU;2-1
Abstract
This paper presents new results about Triton's atmospheric structure f rom the analysis of all ground-based stellar occultation data recorded to date, including one single-chord occultation recorded on 1993 July 10 and nine occultation lightcurves from the double-star event on 199 5 August 14. These stellar occultation observations made both in the v isible and in the infrared have good spatial coverage of Triton, inclu ding the first Triton central-flash observations, and are the first da ta to probe the altitude level 20-100 km on Triton. The small-planet l ightcurve model of J. L. Elliot and L. A, Young (1992, Astron. J. 103, 991-1015) was generalized to include stellar flux refracted by the fa r limb, and then fitted to the data. Values of the pressure, derived f rom separate immersion and emersion chords, show no significant trends with latitude, indicating that Triton's atmosphere is spherically sym metric at similar to 50-km altitude to within the error of the measure ments; however, asymmetry observed in the central flash indicates the atmosphere is not homogeneous at the lowest levels probed (similar to 20-km altitude). From the average of the 1995 occultation data, the eq uivalent-isothermal temperature of the atmosphere is 47 +/- 1 K and th e atmospheric pressure at 1400-km radius (similar to 50-km altitude) i s 1.4 +/- 0.1 mu bar. Both of these are not consistent with a model ba sed on Voyager UVS and RSS observations in 1989 (D. F. Strobel, X. Zhu , M. E. Summers, and M. H. Stevens, 1996, Icarus 120, 266-289). The at mospheric temperature from the occultation is 5 K colder than that pre dicted by the model and the observed pressure is a factor of 1.8 great er than the model. In our opinion, the disagreement in temperature and pressure is probably due to modeling problems at the microbar level, since measurements at this level have not previously been made. Altern atively, the difference could be due to seasonal change in Triton's at mospheric structure. (C) 1997 Academic Press.