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Science 18 October 1996: Vol. 274. no. 5286, pp. 385 - 388 DOI: 10.1126/science.274.5286.385
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Reports
Near-Infrared Spectroscopy and Spectral Mapping of Jupiter
and the Galilean Satellites: Results from Galileo's Initial Orbit
R. Carlson,
*
W. Smythe,
K. Baines,
E. Barbinis,
K. Becker,
R. Burns,
S. Calcutt,
W. Calvin,
R. Clark,
G. Danielson,
A. Davies,
P. Drossart,
T. Encrenaz,
F. Fanale,
J. Granahan,
G. Hansen,
P. Herrera,
C. Hibbitts,
J. Hui,
P. Irwin,
T. Johnson,
L. Kamp,
H. Kieffer,
F. Leader,
E. Lellouch,
R. Lopes-Gautier,
D. Matson,
T. McCord,
R. Mehlman,
A. Ocampo,
G. Orton,
M. Roos-Serote,
M. Segura,
J. Shirley,
L. Soderblom,
A. Stevenson,
F. Taylor,
J. Torson,
A. Weir,
P. Weissman
The Near Infrared Mapping Spectrometer performed spectral
studies of Jupiter and the Galilean satellites during the June 1996 perijove pass of the Galileo spacecraft. Spectra for a 5-micrometer hot
spot on Jupiter are consistent with the absence of a significant water
cloud above 8 bars and with a depletion of water compared to that
predicted for solar composition, corroborating results from the Galileo
probe. Great Red Spot (GRS) spectral images show that parts of this
feature extend upward to 240 millibars, although considerable
altitude-dependent structure is found within it. A ring of dense clouds
surrounds the GRS and is lower than it by 3 to 7 kilometers. Spectra of
Callisto and Ganymede reveal a feature at 4.25 micrometers, attributed
to the presence of hydrated minerals or possibly carbon dioxide on
their surfaces. Spectra of Europa's high latitudes imply that
fine-grained water frost overlies larger grains. Several active
volcanic regions were found on Io, with temperatures of 420 to 620 kelvin and projected areas of 5 to 70 square kilometers.
R. Carlson, W. Smythe, K. Baines, R. Burns, A. Davies, P. Herrera,
J. Hui, T. Johnson, L. Kamp, R. Lopes-Gautier, D. Matson, A. Ocampo, G. Orton, M. Segura, J. Shirley, A. Stevenson, P. Weissman, Jet Propulsion
Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.
E. Barbinis, F. Leader, R. Mehlman, Institute of Geophysics and
Planetary Physics, University of California, Los Angeles, CA 90095, USA.
S. Calcutt, P. Irwin, F. Taylor, A. Weir, Department of Atmospheric,
Oceanic, and Planetary Physics, Oxford University, Oxford OX1 3PU, UK.
K. Becker, W. Calvin, H. Kieffer, L. Soderblom, J. Torson, U.S.
Geological Survey, Flagstaff, AZ 86001, USA.
R. Clark, U.S. Geological Survey, Denver, CO 80225, USA.
G. Danielson, Division of Geological and Planetary Science, California
Institute of Technology, Pasadena, CA 91125, USA.
P. Drossart, T. Encrenaz, E. Lellouch, M. Roos-Serote, Observatoire de
Paris, Meudon 92150, France.
F. Fanale, J. Granahan, G. Hansen, C. Hibbitts, T. McCord, Hawaii
Institute of Geophysics and Planetology, University of Hawaii,
Honolulu, HI 96822, USA.
*
To whom correspondence should be addressed.
Also at SETS Technology, Inc., Mililani, HI 96789, USA.
Read the Full Text
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
- Hydrogen Peroxide on the Surface of Europa.
- R. W. Carlson, M. S. Anderson, R. E. Johnson, W. D. Smythe, A. R. Hendrix, C. A. Barth, L. A. Soderblom, G. B. Hansen, T. B. McCord, J. B. Dalton, et al. (1999)
Science
283, 2062-2064
| Abstract »
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- A Tenuous Carbon Dioxide Atmosphere on Jupiter's Moon Callisto.
- R. W. Carlson (1999)
Science
283, 820-821
| Abstract »
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- Salts on Europa's Surface Detected by Galileo's Near Infrared Mapping Spectrometer.
- T. B. McCord, G. B. Hansen, F. P. Fanale, R. W. Carlson, D. L. Matson, T. V. Johnson, W. D. Smythe, J. K. Crowley, P. D. Martin, A. Ocampo, et al. (1998)
Science
280, 1242-1245
| Abstract »
| Full Text »
- Organics and Other Molecules in the Surfaces of Callisto and Ganymede.
- T. B. McCord, R. W. Carlson, W. D. Smythe, G. B. Hansen, R. N. Clark, C. A. Hibbitts, F. P. Fanale, J. C. Granahan, M. Segura, D. L. Matson, et al. (1997)
Science
278, 271-275
| Abstract »
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- Galileo Photopolarimeter-Radiometer Observations of Jupiter and the Galilean Satellites.
- G. S. Orton, J. R. Spencer, L. D. Travis, T. Z. Martin, and L. K. Tamppari (1996)
Science
274, 389-391
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