NASA Logo

NTRS

NTRS - NASA Technical Reports Server

Back to Results
The origin and vertical distribution of carbon monoxide in JupiterSix clearly-resolved lines of the CO 1-0 vibration-rotation band near 4.7 microns have been observed in Jupiter at a resolution of 0.07/cm. CO is not found to be concentrated in the stratosphere, but is shown to be present in the troposphere at a mole fraction of 1.6 + or - 0.3 x 10 to the -9th, suggesting that rapid vertical mixing is the source of CO. Results indicate that the global oxygen abundance in Jupiter's gaseous envelope below the cloud-forming regions must be near the solar value, and that intervening clouds with an optical depth of 0.5-4 are present above the line-forming region.
Document ID
19880038126
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
External Source(s)
Authors
Noll, Keith S.
(State Univ. of New York Stony Brook, NY, United States)
Knacke, R. F.
(New York, State University Stony Brook, United States)
Geballe, T. R.
(Edinburgh, Royal Observatory, U.K. Infrared Telescope Unit, Hilo, HI; Stichting Astronomisch Onderzoek in Nederland Amsterdam, Netherlands)
Tokunaga, A. T.
(Hawaii, University Honolulu, United States)
Date Acquired
August 13, 2013
Publication Date
January 15, 1988
Publication Information
Publication: Astrophysical Journal, Part 1
Volume: 324
ISSN: 0004-637X
Subject Category
Lunar And Planetary Exploration
Accession Number
88A25353
Funding Number(s)
CONTRACT_GRANT: NSG-7286
CONTRACT_GRANT: NGT-33-015-803
Distribution Limits
Public
Copyright
Other

Available Downloads

There are no available downloads for this record.
No Preview Available