Electron scattering by magnetosonic waves in the inner magnetosphere

Journal Article · Mon Dec 28 00:00:00 UTC 2015 · Journal of Geophysical Research. Space Physics

DOI:https://doi.org/10.1002/2015JA021992· OSTI ID:1467662

Ma, Qianli ^[1]; Li, Wen ^[2]; Thorne, Richard M. ^[2]; Bortnik, Jacob ^[2]; Kletzing, C. A. ^[3]; Kurth, W. S. ^[3]; Hospodarsky, G. B. ^[3]

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1. Univ. of California, Los Angeles, CA (United States); Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, California
2. Univ. of California, Los Angeles, CA (United States)
3. Univ. of Iowa, Iowa City, IA (United States)

Here, we investigate the importance of electron scattering by magnetosonic waves in the Earth’s inner magnetosphere. A statistical survey of the magnetosonic wave amplitude and wave frequency spectrum, as a function of geomagnetic activity, is performed using the Van Allen Probes wave measurements and is found to be generally consistent with the wave distribution obtained from previous spacecraft missions. Outside the plasmapause the statistical frequency distribution of magnetosonic waves follows the variation of the lower hybrid resonance frequency, but this trend is not observed inside the plasmasphere. Drift and bounce averaged electron diffusion rates due to magnetosonic waves are calculated using a recently developed analytical formula. The resulting timescale of electron energization during disturbed conditions (when AE* > 300 nT) is more than 10 days. We perform a 2-D simulation of the electron phase space density evolution due to magnetosonic wave scattering during disturbed conditions. Outside the plasmapause, the waves accelerate electrons with pitch angles between 50° and 70° and form butterfly pitch angle distributions at energies from ~100 keV to a few MeV over a timescale of several days; whereas inside the plasmapause, the electron acceleration is very weak. Our study suggests that intense magnetosonic waves may cause the butterfly distribution of radiation belt electrons especially outside the plasmapause, but electron acceleration due to magnetosonic waves is generally not as effective as chorus wave acceleration.

• Research Organization: Univ. of California, Los Angeles, CA (United States)
• Sponsoring Organization: USDOE Office of Science (SC)
• Grant/Contract Number: SC0010578
• OSTI ID: 1467662
• Journal Information: Journal of Geophysical Research. Space Physics, Journal Name: Journal of Geophysical Research. Space Physics Journal Issue: 1 Vol. 121; ISSN 2169-9380
• Publisher: American Geophysical Union
• Country of Publication: United States
• Language: English

Related Subjects

79 ASTRONOMY AND ASTROPHYSICS
Van Allen Probes statistics
electron scattering
magnetosonic waves