HEATING OF PROTON CONICS BY RESONANT ABSORPTION IN A MULTICOMPONENT PLASMA .1. EXPERIMENTAL-EVIDENCE

被引:24
作者
RAUCH, JL
LEFEUVRE, F
LEQUEAU, D
ROUX, A
BOSQUED, JM
BERTHELIER, JJ
机构
[1] LAB PHYS & CHIM ENVIRONNEMENT, CNRS, 3A AVE RECH SCI, F-45071 ORLEANS 2, FRANCE
[2] CTR NATL ETUDE TELECOMMUN, CTR RECH PHYS ENVIRONNEMENT, CNRS, F-94107ST MAUR FOSSES, FRANCE
[3] CTR ETUDE SPATIAL RAYONNEMENTS, CNRS, F-31029 TOULOUSE, FRANCE
[4] CTR RECH PHYS ENVIRONN, ENTITE CTR RECH SCI, F-78140 VELIZY VILLACOUBLAY, FRANCE
[5] CTR NATL ETUD TELECOMMUN, CTR RECH PHYS ENVIRONNEMENT, CNRS, F-92131 ISSY LES MOULINEAX, FRANCE
关键词
D O I
10.1029/92JA02255
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
ELF emissions observed on the low-altitude AUREOL 3 satellite are seen in association with H+ ions at large pitch angle. The flux in the upward direction for approximately 120-degrees pitch angle is found to be equal to or larger than the flux at approximately 60-degrees pitch angle, which provides evidence for transverse acceleration at or below the spacecraft. These emissions have a sharp lower-frequency cutoff of the transverse components of the electric field and a narrow peak at, or, more precisely, just below the proton gyrofrequency f(H)+. This narrow peak is more easily seen on the parallel component and appears as a narrow line on the spectrogram of this component. A statistical study of the occurrence of this line at f approximately f(H)+ is presented. It is shown that this line is observed at relatively high invariant latitude within the light ion trough where a strong depletion of thermal H+ ions occurs. Detailed analysis of ELF waves observed just below f(H)+ demonstrates that they propagate in the left-hand mode. These observations are interpreted as a signature of mode conversion from a fast magnetosonic mode into a slow proton cyclotron mode. It is suggested that this slow proton cyclotron wave can accelerate protons up to a few hundreds electron volts in the transverse direction. This mode conversion process can operate over a much broader of large altitude range than covered by AUREOL 3; it is a likely candidate for explaining the formation of H+ conics. Theoretical calculations that support the above conclusions are given in a companion paper by Le Queau et al. (this issue).
引用
收藏
页码:13347 / 13361
页数:15
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