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Title: Whistler mode noise in Jupiter's inner magnetosphere

Journal Article · · J. Geophys. Res.; (United States)

The distinctive 'hat shape' of equatorial pitch angle distributions constructed from Pioneer 10 and 11 Jupiter observations of energetic electrons E/sub e/>21 MeV and E/sub e/>31 MeV at L=3 is examined from the point of view of pitch angle diffusion by resonant interaction with a band-limited spectrum of whistler mode noise. In this picture, the pitch angle profiles are consistent with whistler mode noise limited to frequencies below an upper cutoff frequency 2.8< or approx. =..integral../sub c/< or approx. =4.6kHz. Equatorial linear growth 3<10 using previously published models for the spatial distribution of thermal plasma and the energetic electron distributions. The maximum frequency for which wave growth is positive at L=3 is roughly consistent with that implied by the 21- and 31-MeV equatorial pitch angle profiles. Maximum growth rates computed from the respective energetic electron models span the range 0.1< or approx. =..gamma../sub max/< or approx. =10 s/sup -1/ throughout the inner region. The spectral extent of the whistler mode noise, defined by those frequencies for which ..gamma..>0.5..gamma../sub max,/ is approximately 2--10 kHz a L=3 and falls smoothly to 0.2--2 kHz at L =10. Raytracing of nonducted whistlers of characteristic frequencies 1-4 kHz generated at the magnetic equator and propagated through a finite temperature (100--400 eV) hydrogen plasma cengrifugally confined near the magnetic equatorial plane shows that wave phase speed decrease to near or below electron thermal speeds before high-latitude reflection can occur. Wave growth in this case is limited to a disclike region centered about the magnetic equator. The amplitude growth of the most unsable whistlers propagating across the growth region parallel to the magnetic field is approx.exp (3--4).

Research Organization:
Department of Physics and Astronomy, University of Iowa, Iowa City, Iowa 52242
OSTI ID:
6673813
Journal Information:
J. Geophys. Res.; (United States), Vol. 83:A7
Country of Publication:
United States
Language:
English