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Collisional electrostatic ion cyclotron waves as a possible source of energetic heavy ions in the magnetosphere

Journal Article · · Journal of Geophysical Research; (United States)
 [1];  [2]
  1. Mitre Corp., Bedford, MA (United States)
  2. Cornell Univ., Ithaca, NY (United States)
A new mechanism is proposed for the source of energetic heavy ions (NO{sup +}, O{sub 2}{sup +}, and O{sup +}) found in the magnetosphere. Simulations using a multispecies particle simulation code for resistive current-driven electrostatic ion cyclotron waves show transverse and parallel bulk heating of bottomside ionospheric NO{sup +}, O{sub 2}{sup +} and O{sup +} ion populations. The dominant mechanism for the transverse bulk heating is resonant ion heating by wave-particle ion trapping. Using a linear kinetic dispersion relation for a magnetized, collisional, homogeneous, and multi-ion plasma, it is found that collisional electrostatic ion cyclotron waves near the NO{sup +}, O{sub 2}{sup +}, and O{sup +} gyrofrequencies are unstable to field-aligned currents of 50 {mu} A/m{sup 2} for a typical bottomside ionosphere (<300 km altitude). A simple ion outflow model of heavy ions is formulated that verifies the assertion that a large number of energetic heavy ions originating from below 250 km can reach the topside ionosphere (> 1000 km), and then via parallel electric fields be ejected into the Earth's magnetosphere.
OSTI ID:
5221911
Journal Information:
Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 95:A4; ISSN 0148-0227; ISSN JGREA
Country of Publication:
United States
Language:
English