1968Journal of Geophysical Research AtmospheresOpen access

Identification of moving magnetic field lines

T. J. Birmingham, F. C. Jones

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Abstract

Magnetic field line motion and its relationship with particle E × B drifts are considered. It is shown that a unique and significant field line identification can be made whenever all field lines in a region pierce a conducting, but arbitrarily shaped surface. If the region in question is free space, particle electric drifts, in general, bear no relation with field line motion identified in this fashion. However, with a conducting plasma filling the region and allowing no parallel component of electric field ( E·B = 0), particles drift so as to always remain on the same magnetic line of force. These points are specifically illustrated for a time-dependent model of the earth's magnetosphere.

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What this paper is about

Magnetic field line motion and its relationship with particle E × B drifts are considered. It is shown that a unique and significant field line identification can be made whenever all field lines in a region pierce a conducting, but arbitrarily shaped surface. If the region in question is free space, particle electric drifts, in general, bear no relation with field line motion identified in this fashion. However, with a conducting plasma filling the region and allowing no parallel component of electric field ( E·B = 0), particles drift so as to always remain on the same magnetic line of force. These points are specifically illustrated for a time-dependent model of the earth's magnetosphere.

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Available abstract

Magnetic field line motion and its relationship with particle E × B drifts are considered. It is shown that a unique and significant field line identification can be made whenever all field lines in a region pierce a conducting, but arbitrarily shaped surface. If the region in question is free space, particle electric drifts, in general, bear no relation with field line motion identified in this fashion. However, with a conducting plasma filling the region and allowing no parallel component of electric field ( E·B = 0), particles drift so as to always remain on the same magnetic line of force. These points are specifically illustrated for a time-dependent model of the earth's magnetosphere.

Key concepts: Field line, Magnetosphere particle motion, Magnetosphere, Electric field, Physics, Magnetic field, Line (geometry), Field (mathematics)

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