Cassini Dust Measurements at Enceladus and Implications for the Origin of the E Ring
Author(s) -
F. Spahn,
Jürgen Schmidt,
N. Albers,
Marcel Hörning,
Martin Makuch,
M. Seiß,
S. Kempf,
R. Srama,
V. Dikarev,
S. Helfert,
G. MoragasKlostermeyer,
A. V. Krivov,
M. Sremčević,
A. J. Tuzzolino,
T. Economou,
E. Grün
Publication year - 2006
Publication title -
science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 12.556
H-Index - 1186
eISSN - 1095-9203
pISSN - 0036-8075
DOI - 10.1126/science.1121375
Subject(s) - enceladus , saturn , astrobiology , production rate , polar , cosmic dust , physics , icy moon , satellite , interplanetary dust cloud , spacecraft , astronomy , environmental science , planet , solar system , industrial engineering , engineering
During Cassini's close flyby of Enceladus on 14 July 2005, the High Rate Detector of the Cosmic Dust Analyzer registered micron-sized dust particles enveloping this satellite. The dust impact rate peaked about 1 minute before the closest approach of the spacecraft to the moon. This asymmetric signature is consistent with a locally enhanced dust production in the south polar region of Enceladus. Other Cassini experiments revealed evidence for geophysical activities near Enceladus' south pole: a high surface temperature and a release of water gas. Production or release of dust particles related to these processes may provide the dominant source of Saturn's E ring.
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