Case studies on the wave propagation and polarization of ELF emissions observed by Freja around the local proton gyrofrequency

Citation
O. Santolik et M. Parrot, Case studies on the wave propagation and polarization of ELF emissions observed by Freja around the local proton gyrofrequency, J GEO R-S P, 104(A2), 1999, pp. 2459-2475
Citations number
36
Categorie Soggetti
Space Sciences
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
ISSN journal
21699380 → ACNP
Volume
104
Issue
A2
Year of publication
1999
Pages
2459 - 2475
Database
ISI
SICI code
0148-0227(19990201)104:A2<2459:CSOTWP>2.0.ZU;2-2
Abstract
Using a multicomponent measurement of electric and magnetic fields in the E LF range, we investigate the polarization and propagation characteristics o f several types of electromagnetic emissions around the local proton gyrofr equency. The data of the low-orbiting Freja satellite are examined in the a uroral and subauroral regions as well as inside the plasmasphere. We confir m previous results on the properties of the high-latitude hiss with a sharp lower cutoff just below the local proton gyrofrequency. The waves propagat e downward from higher altitudes outside the plasmasphere and reflect at th e local two-ion cutoff frequency. With an enhanced data representation we a re able to characterize the reflected upgoing waves on both poleward and eq uatorward edges of the hiss emission. The high-latitude emissions in a larg e band below the local proton gyrofrequency contain right-hand circularly p olarized waves propagating nearly parallel to the terrestrial magnetic fiel d. We believe these emissions can originate by tunnelling of the right-hand -polarized hiss below the two-ion crossover frequency. We report high-latit ude "frequency drift phenomena" below the local proton gyrofrequency. The f requency of these faint emissions increases by several tens of hertz per la titude degree. The electromagnetic noise at low frequencies is always found with a high degree of a nearly linear polarization. Upgoing ion whistlers are observed to follow each other with time delays as low as about 100 ms.