Hostname: page-component-848d4c4894-tn8tq Total loading time: 0 Render date: 2024-06-24T04:26:57.161Z Has data issue: false hasContentIssue false

The effective temperature of Jupiter'S equatorial belt during the 1965 apparition

Published online by Cambridge University Press:  14 August 2015

L. M. Trafton
Affiliation:
University of Texas at Austin, Austin, Tex., U.S.A.
R. Wildey
Affiliation:
U.S. Geological Survey, Center of Astrogeology, Flagstaff, Ariz., U.S.A.

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Preliminary results from our study of Jupiter's equatorial limb darkening at 8–14 μ indicate that the effective temperature of the equatorial belt lay between 140 K and 150 K. We find these temperatures to be insensitive to the likely range of the He/H2 ratios. These results assume that Jupiter's only significant sources of extinction at these wavelengths are the pressure-induced absorption of H2 and He and the absorption of saturated NH3.

Type
Part III: Outer Planets
Copyright
Copyright © Reidel 1971 

References

France, W. L. and Williams, D.: 1966, J. Opt. Soc. Amer. 56, 70.Google Scholar
Garing, J. S., Nielson, H. H., and Rao, K. N.: 1959, J. Molecular Spectrosc. 3, 496.Google Scholar
Giver, L.: 1968, private communication.Google Scholar
Howard, R. and Smith, W. V.: 1950, Phys. Rev. 79, 132.Google Scholar
Landenburg, R. W. and Reiche, F.: 1913, Ann. Phys. 42, 181.Google Scholar
Mould, H. M., Price, W. C., and Wilkinson, G. R.: 1959, Spectrochim. Acta 15, 314.Google Scholar
Townes, C. H. and Schawlow, A. L.: 1955, in Microwave Spectroscopy, New York, Chapters 12–13.Google Scholar
Trafton, L. M.: 1967, Astrophys. J. 147, 765.Google Scholar
Wildey, R. L.: 1966, Z. Astrophys. 64, 32.Google Scholar
Wildey, R. L.: 1968, Astrophys. J. 154, 761.Google Scholar