Sublimation in bright spots on (1) Ceres
A. Nathues (),
M. Hoffmann,
M. Schaefer,
L. Le Corre,
V. Reddy,
T. Platz,
E. A. Cloutis,
U. Christensen,
T. Kneissl,
J.-Y. Li,
K. Mengel,
N. Schmedemann,
T. Schaefer,
C. T. Russell,
D. M. Applin,
D. L. Buczkowski,
M. R. M. Izawa,
H. U. Keller,
D. P. O’Brien,
C. M. Pieters,
C. A. Raymond,
J. Ripken,
P. M. Schenk,
B. E. Schmidt,
H. Sierks,
M. V. Sykes,
G. S. Thangjam and
J.-B. Vincent
Additional contact information
A. Nathues: Max Planck Institute for Solar System Research
M. Hoffmann: Max Planck Institute for Solar System Research
M. Schaefer: Max Planck Institute for Solar System Research
L. Le Corre: Max Planck Institute for Solar System Research
V. Reddy: Max Planck Institute for Solar System Research
T. Platz: Max Planck Institute for Solar System Research
E. A. Cloutis: University of Winnipeg
U. Christensen: Max Planck Institute for Solar System Research
T. Kneissl: Freie Universitaet Berlin
J.-Y. Li: Planetary Science Institute
K. Mengel: Technische Universitaet Clausthal
N. Schmedemann: Freie Universitaet Berlin
T. Schaefer: Max Planck Institute for Solar System Research
C. T. Russell: University of California, Los Angeles (UCLA)
D. M. Applin: University of Winnipeg
D. L. Buczkowski: Johns Hopkins University
M. R. M. Izawa: University of Winnipeg
H. U. Keller: TU Braunschweig
D. P. O’Brien: Planetary Science Institute
C. M. Pieters: Brown University
C. A. Raymond: Jet Propulsion Laboratory
J. Ripken: Max Planck Institute for Solar System Research
P. M. Schenk: Lunar and Planetary Institute
B. E. Schmidt: Georgia Institute of Technology
H. Sierks: Max Planck Institute for Solar System Research
M. V. Sykes: Planetary Science Institute
G. S. Thangjam: Max Planck Institute for Solar System Research
J.-B. Vincent: Max Planck Institute for Solar System Research
Nature, 2015, vol. 528, issue 7581, 237-240
Abstract:
The dwarf planet (1) Ceres, the largest object in the main asteroid belt, is found to have localized bright areas on its surface; particularly interesting is a bright pit on the floor of the crater Occator that exhibits what is likely to be water ice sublimation, producing crater-bound haze clouds with a diurnal rhythm.
Date: 2015
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Persistent link: https://EconPapers.repec.org/RePEc:nat:nature:v:528:y:2015:i:7581:d:10.1038_nature15754
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DOI: 10.1038/nature15754
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