Local transverse ion energization in and near the polar cusp

Journal Article · Fri Jan 01 04:00:00 EST 1988 · Geophys. Res. Lett.; (United States)

DOI:https://doi.org/10.1029/GL015i001p00107· OSTI ID:5331562

Andre, M; Koskinen, H; Matson, L; Erlandson, R

Ion conics are often observed in the dayside polar cusp region of the magnetosphere by the polar orbiting Viking satellite. These ion distributions may be locally heated perpendicularly to the ambient magnetic field to temperatures of about 100 eV. The conics are closely associated with increased electron fluxes but may occur equatorward of the region of ions injected from the magnetosheath. They are also closely related to waves with frequencies up to about 100 Hz. The wave electric field is directed mainly perpendicular to the ambient magnetic field and shows no clear structure near the ion gyrofrequencies or their harmonics. Observations of ion conics at 90/sup 0/ pitch angle and the related waves indicate that the waves may cause significant ion heating, especially of heavy ions. copyright American Geophysical Union 198

• Research Organization: Swedish Institute of Space Physics
• OSTI ID: 5331562
• Journal Information: Geophys. Res. Lett.; (United States), Journal Name: Geophys. Res. Lett.; (United States) Vol. 15:1; ISSN GPRLA
• Country of Publication: United States
• Language: English

Related Subjects

640201* -- Atmospheric Physics-- Auroral
Ionospheric
& Magetospheric Phenomena
71 CLASSICAL AND QUANTUM MECHANICS
GENERAL PHYSICS
CHARGED PARTICLES
CONES
EARTH ATMOSPHERE
EARTH MAGNETOSPHERE
ELECTRIC FIELDS
ELECTRON DRIFT
ENERGY LEVELS
HEATING
HEAVY IONS
ION TEMPERATURE
IONS
MAGNETIC FIELD CONFIGURATIONS
PLASMA WAVES
POLAR CUSP