Plasma turbulence disc circulating the equatorial region of the plasmasphere identified by the plasma wave detector (PWS) onboard the Akebono (EXOS-D) satellite

Details Plasma turbulence disc circulating the equatorial region of the plasmasphere identified by the plasma wave detector (PWS) onboard the Akebono (EXOS-D) satellite Plasma turbulence disc circulating the equatorial region of the plasmasphere identified by the plasma wave detector (PWS) onboard the Akebono (EXOS-D) satellite

Feb 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991georl..18..329o&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 18, Feb. 1991, p. 329-332.

Computer Science

Sound

5

Equatorial Atmosphere, Exos-D Satellite, Plasma Turbulence, Plasma Waves, Plasmasphere, Satellite Sounding, Electric Fields, Exos Satellites, Plasma Drift, Plasmapause, Vertical Distribution

Scientific paper

For the observation data of the plasma wave turbulence detected by the PWS (Plasma Wave and Sounder Experiment) on board the EXOS-D (Akebono) satellite, the enhancements of the upper hybrid wave emission called equatorial enhancement of the plasma wave turbulence (EPWAT) that are characterized by the increasing level of the upper hybrid emissions are studied on their occurrence regions and occurrence conditions. The results show that EPWAT's encircle the magnetic equator forming a disk region that spreads from 1000 km to 10,000 km altitude without dependence on the local time. The generation of plasma wave turbulences, EPWAT's are possibly controlled by the plasma drift as principal source in the region of the magnetic equator due to existing electric field.

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