z-logo
open-access-imgOpen Access
Relativistic electron precipitation during magnetic storm main phase
Author(s) -
Thorne R. M.,
Kennel C. F.
Publication year - 1971
Publication title -
journal of geophysical research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/ja076i019p04446
Subject(s) - electron precipitation , storm , geomagnetic storm , electron , precipitation , phase (matter) , geophysics , van allen radiation belt , physics , atmospheric sciences , geology , magnetosphere , meteorology , plasma , nuclear physics , solar wind , quantum mechanics
Relativistic electrons can have cyclotron resonances with electromagnetic ion‐cyclotron waves. The resonant energy is generally well above 1 Mev throughout the magnetosphere, but it can fall to near 1 Mev just within the plasmapause. This also corresponds to the region where ring current (10–50 kev) protons are expected to be strongly unstable. The resulting ion‐cyclotron wave amplitude necessary to precipitate ring current protons leads to electron lifetimes near the strong diffusion limit. Thus, >1‐Mev electrons whose drift orbits intersect the stormtime plasmapause should rapidly be precipitated in the region 3< L <5 during the initial phase of a magnetic storm.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom