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Identifying the source region of plasmaspheric hiss
Author(s) -
Laakso Harri,
Santolik Ondrej,
Horne Richard,
Kolmasová Ivana,
Escoubet Philippe,
Masson Arnaud,
Taylor Matthew
Publication year - 2015
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2015gl063755
Subject(s) - plasmasphere , hiss , equator , geophysics , van allen radiation belt , geology , magnetic dip , physics , van allen probes , magnetosphere , magnetic field , geodesy , latitude , electron , quantum mechanics
The presence of the plasmaspheric hiss emission around the Earth has been known for more than 50 years, but its origin has remained unknown in terms of source location and mechanism. The hiss, made of whistler mode waves, exists for most of the time in the plasmasphere and is believed to control the radiation belt surrounding the Earth which makes its understanding very important. This paper presents direct observational evidence that the plasmaspheric hiss originates in the equatorial region of the plasmaspheric drainage plumes. It shows that the emissions propagate along the magnetic field lines and away from the equator in the plumes but toward the equator at lower L shells inside the plasmasphere. The observations also suggest that the hiss waves inside the plasmasphere are absorbed as they cross the equator.