Potential waves for relativistic electron scattering and stochastic acceleration during magnetic storms

The possibility of electron stochastic energization to relativisitic energies (≥ 1 MeV) via resonant wave-particle interactions during a magnetic storm is explored. The minimum electron energy Emin for cyclotron resonant interaction with various electromagnetic waves is calculated for conditions representative of storm-times. Since Emin > 1 MeV for resonance with L-mode ion cyclotron waves, intense stormtime EMIC waves could contribute to relativistic electron loss, but not acceleration. Inside the plasmapause whistler mode waves, and highly oblique magnetosonic waves near the lower hybrid frequency, can resonate with electrons over the important energy range from ∼ 100 keV to ∼ 1 MeV. In low density regions outside the plasmapause, the whistler, RX, LO and Z modes can resonate with electrons over a similar energy range. These waves have the potential to contribute to the stochastic acceleration of electrons up to relativistic energies during magnetic storms.

[1]  J. B. Blake,et al.  Dynamics of the outer radiation belt , 1997 .

[2]  Richard M. Thorne,et al.  On the preferred source location for the convective amplification of ion cyclotron waves , 1993 .

[3]  D. Baker,et al.  Are energetic electrons in the solar wind the source of the outer radiation belt? , 1997 .

[4]  C. Kennel,et al.  Relativistic electron precipitation during magnetic storm main phase , 1971 .

[5]  J. B. Blake,et al.  Correlation of changes in the outer‐zone relativistic‐electron population with upstream solar wind and magnetic field measurements , 1997 .

[6]  R. Horne Path-integrated growth of electrostatic waves: The generation of terrestrial myriametric radiation , 1989 .

[7]  Lou‐Chuang Lee,et al.  A theory of the terrestrial kilometric radiation , 1979 .

[8]  D. Baker,et al.  Relativistic electrons near geostationary orbit: Evidence for internal magnetospheric acceleration , 1989 .

[9]  B. Tsurutani,et al.  Plasmaspheric hiss intensity variations during magnetic storms , 1974 .

[10]  J. B. Blake,et al.  Relativistic Electron Acceleration and Decay Time Scales in the Inner and Outer Radiation Belts: SAMPEX , 1994 .

[11]  A. Roux,et al.  A systematic study of ULF Waves Above FH+ from GEOS 1 and 2 Measurements and Their Relationships with proton ring distributions , 1982 .

[12]  J. Green,et al.  Funnel‐shaped, low‐frequency equatorial waves , 1992 .

[13]  R. Thorne,et al.  Relativistic theory of wave‐particle resonant diffusion with application to electron acceleration in the magnetosphere , 1998 .

[14]  D. Baker,et al.  Multisatellite observations of the outer zone electron variation during the November 3–4, 1993, magnetic storm , 1997 .

[15]  R. Horne,et al.  Landau damping of magnetospherically reflected whistlers , 1994 .

[16]  A. Roux,et al.  Magnetosonic waves above fc (H+) at geostationary orbit: GEOS 2 results , 1990 .