AN ANALYSIS OF NEPTUNE STRATOSPHERIC HAZE USING HIGH-PHASE-ANGLE VOYAGER IMAGES

Citation
Ji. Moses et al., AN ANALYSIS OF NEPTUNE STRATOSPHERIC HAZE USING HIGH-PHASE-ANGLE VOYAGER IMAGES, Icarus, 113(2), 1995, pp. 232-266
Citations number
60
Categorie Soggetti
Astronomy & Astrophysics
Journal title
IcarusACNP
ISSN journal
00191035
Volume
113
Issue
2
Year of publication
1995
Pages
232 - 266
Database
ISI
SICI code
0019-1035(1995)113:2<232:AAONSH>2.0.ZU;2-H
Abstract
We have inverted high-phase-angle Voyager images of Neptune to determi ne the atmospheric extinction coefficient as a function of altitude an d the scattering phase function at a reference altitude. Comparisons b etween theoretical models and observations help separate the contribut ions from molecular Rayleigh and aerosol scattering and help determine the variation of the aerosol size, concentration, and scattering prop erties with altitude. Further comparisons between models and data allo w us to place constraints on the location and composition of the hazes , the concentration and downward Bur of certain condensible hydrocarbo n gases, the eddy diffusion coefficient in the lower stratosphere, and the thermal profile in parts of Neptune's stratosphere. We find that a distinct stratospheric haze layer exists near 12(-1)(+1) mbar in Nep tune's lower stratosphere, most probably due to condensed ethane, The derived stratospheric haze production rate of 1.0(-0.3)(+0.2) x 10(-15 ) g cm(-2) sec(-1) is substantially lower than photochemical model pre dictions. Evidence for hazes at higher altitudes also exists. Unlike t he situation on Uranus, large particles (0.08-0.11 mu m) may be presen t at high altitudes on Neptune (e.g., near 0.5 mbar), well above the r egion in which we expect the major hydrocarbon species to condense. Ne ar 28 mbar, the mean particle size is about 0.13(-0.02)(+0.02) mu m wi th a concentration of 5(-3)(+3) particles cm(-3). The cumulative haze extinction optical depth above 15 mbar in the clear filter is similar to 3 x 10(-3), and much of this extinction is due to scattering rather than absorption; thus, if our limb-scan sites are typical, the hazes cannot account for the stratospheric temperature inversion on Neptune and may not contribute significantly to atmospheric heating. We compar e the imaging results with the results from other,observations, includ ing those of the Voyager Photopolarimeter Subsystem, and discuss diffe rences between Neptune and Uranus. (C) 1995 Academic Press, Inc.