Premium
Correction to “Interchange instability in the inner magnetosphere associated with geosynchronous particle flux decreases”
Author(s) -
Sazykin S.,
Wolf R. A.,
Spiro R. W.,
Gombosi T. I.,
DeZeeuw D. L.,
Thomsen M. F.
Publication year - 2004
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2003gl019191
Subject(s) - magnetosphere , instability , physics , flux (metallurgy) , context (archaeology) , geosynchronous orbit , scaling , geophysics , computational physics , mathematics , geometry , geology , nuclear physics , mechanics , chemistry , astronomy , plasma , satellite , paleontology , organic chemistry
[1] We simulate the inner magnetosphere during the magnetic storm of September 25, 1998 using the Rice Convection Model with boundary fluxes estimated from geosynchronous data. Model results indicate development of an interchange-like instability in the dusk-to-midnight sector, producing ripple structures in the plasma density, swirls in the subauroral ionospheric electric field pattern, and undulations near the equatorward edge of the diffuse aurora. We suggest that these disturbances might be observable whenever a strong main-phase ring-current injection is followed by a major, sustained decrease in the plasma energy density at geosynchronous orbit, a circumstance that will also produce rapid decay of the storm-time ring current.