MESSENGER Observations of Extreme Loading and Unloading of Mercury’s Magnetic Tail
Author(s) -
J. A. Slavin,
B. J. Anderson,
D. N. Baker,
M. Benna,
S. A. Boardsen,
G. Gloeckler,
R. E. Gold,
G. C. Ho,
H. Korth,
S. M. Krimigis,
R. L. McNutt,
L. R. Nittler,
J. M. Raines,
M. Sarantos,
D. Schriver,
Sean C. Solomon,
R. Starr,
P. Trávnı́ček,
T. H. Zurbuchen
Publication year - 2010
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.1188067
Subject(s) - mercury (programming language) , exosphere , magnetosphere , planet , mercury's magnetic field , physics , astrobiology , solar wind , geophysics , volcano , ionosphere , magnetic field , astrophysics , geology , ion , interplanetary magnetic field , quantum mechanics , computer science , programming language , seismology
During MESSENGER's third flyby of Mercury, the magnetic field in the planet's magnetic tail increased by factors of 2 to 3.5 over intervals of 2 to 3 minutes. Magnetospheric substorms at Earth are powered by similar tail loading, but the amplitude is lower by a factor of approximately 10 and typical durations are approximately 1 hour. The extreme tail loading observed at Mercury implies that the relative intensity of substorms must be much larger than at Earth. The correspondence between the duration of tail field enhancements and the characteristic time for the Dungey cycle, which describes plasma circulation through Mercury's magnetosphere, suggests that such circulation determines the substorm time scale. A key aspect of tail unloading during terrestrial substorms is the acceleration of energetic charged particles, but no acceleration signatures were seen during the MESSENGER flyby.
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