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Title: Formation of low-energy trapped and field-aligned ion distributions in substorm dipolarization events

Journal Article · · Journal of Geophysical Research
DOI:https://doi.org/10.1029/95JA03217· OSTI ID:255032
;  [1]
  1. Univ. of Alabama, Huntsville, AL (United States)

A dynamic semikinetic simulation is used to study the effect of substorm dipolarization events on low-energy thermal plasmas initially distributed isotropically along closed tailward stretched magnetic field lines in the middle magnetosphere. The temporal variation of the magnetic field during dipolarization induces a perpendicular electric field that leads to E x B drift and produces centrifigural and betatron ion acceleration. The authors find that the dipolarization process produces field-aligned ion streams split into components with higher and lower speeds, as generated by parallel forces identified here as the {open_quotes}centrifugal force{close_quotes} and the {open_quotes}Coriolis force{close_quotes}. The higher-speed component leads to ion precipitation which is highly dispersed in energy during the dipolarization event. The post dipolarization evolution of the lower-speed component produces energy-time spectogram features similiar to the {open_quotes}ion bounce clusters{close_quotes} observed at geosynchronous orbit noted in the {open_quotes}convection surge{close_quotes} simulations of Mauk. An entirely new feature not found in previous dipolarization simulations is the formation of an equatorially trapped population whose flux is strongly peaked at the 90{degrees} pitch angle and whose overall level sharply declines at latitudinal boundaries within 5{degrees} of the equator. These equatorially trapped ion distributions are generated through the combined influence of equatorial focusing by the parallel centrifugal force and betatron perpendicular energization. The postdipolarization latitudinal density distributions contain a local maximum, due to the trapped ion population, at the equator, where the electric potential similarly contains a small peak. Hence the substorm dipolarization process provides a new, heretofore unrecognized mechanism for producing the characteristic equatorially trapped warm ion populations. 35 refs., 9 figs.

OSTI ID:
255032
Journal Information:
Journal of Geophysical Research, Vol. 101, Issue A3; Other Information: PBD: 1 Mar 1996
Country of Publication:
United States
Language:
English

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