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Near‐Earth breakup triggered by the earthward traveling burst flow
Author(s) -
Voronkov I. O.
Publication year - 2005
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 - 10.1029/2005gl022983
Subject(s) - breakup , physics , magnetic field , convection , geophysics , plasma sheet , plasma , nonlinear system , leading edge , computational physics , mechanics , magnetosphere , quantum mechanics
Computer modeling is performed in order to explore a hypothesis stating that the near‐Earth breakup can be triggered by a pulse of convection traveling earthward from the more distant magnetotail. The following possible scenario for the interaction of the burst with the near‐Earth edge of the plasma sheet (PS) is revealed. The near‐dipolar magnetic field topology of the inner PS leads to the flow breaking which in turn launches a wide spectrum of dispersive compressional waves propagating further Earthward. Strong topological variations of the magnetic field at the inner edge of the PS, required by the equilibrium conditions, play a role of the resonant cavity for selected compressional modes. Growing resonance modes provide a ponderomotive force pumping up corresponding nonlinear ballooning eigenmodes. The latter extract energy stored in the inner PS and produce vortical structures expanding tailward.