Journal article
Quantitative Evaluation of Radial Diffusion and Local Acceleration Processes During GEM Challenge Events
Journal of geophysical research. Space physics, Vol.123(3), pp.1938-1952
03/2018
DOI: 10.1002/2017JA025114
Abstract
We simulate the radiation belt electron flux enhancements during selected Geospace Environment Modeling (GEM) challenge events to quantitatively compare the major processes involved in relativistic electron acceleration under different conditions. Van Allen Probes observed significant electron flux enhancement during both the storm time of 17–18 March 2013 and non–storm time of 19–20 September 2013, but the distributions of plasma waves and energetic electrons for the two events were dramatically different. During 17–18 March 2013, the SYM‐H minimum reached −130 nT, intense chorus waves (peak Bw ~140 pT) occurred at 3.5 < L < 5.5, and several hundred keV to several MeV electron fluxes increased by ~2 orders of magnitude mostly at 3.5 < L < 5.5. During 19–20 September 2013, the SYM‐H remained higher than −30 nT, modestly intense chorus waves (peak Bw ~80 pT) occurred at L > 5.5, and electron fluxes at energies up to 3 MeV increased by a factor of ~5 at L > 5.5. The two electron flux enhancement events were simulated using the available wave distribution and diffusion coefficients from the GEM focus group Quantitative Assessment of Radiation Belt Modeling. By comparing the individual roles of local electron heating and radial transport, our simulation indicates that resonant interaction with chorus waves is the dominant process that accounts for the electron flux enhancement during the storm time event particularly near the flux peak locations, while radial diffusion by ultralow‐frequency waves plays a dominant role in the enhancement during the non–storm time event. Incorporation of both processes reasonably reproduces the observed location and magnitude of electron flux enhancement.
Key Points
Energetic electron fluxes are enhanced during storm and non–storm time events, but wave and electron structures are dramatically different
Local heating by whistler mode chorus wave is the major contributor to the flux enhancement near the peak during 17–18 March 2013
Radial diffusion by ultralow‐frequency wave is the major contributor to the observed flux enhancement during 19–20 September 2013
Details
- Title: Subtitle
- Quantitative Evaluation of Radial Diffusion and Local Acceleration Processes During GEM Challenge Events
- Creators
- Q Ma - Boston UniversityW Li - Boston UniversityC. A Kletzing - University of IowaW. S Kurth - University of IowaJ Bortnik - University of California, Los AngelesG. B Hospodarsky - University of IowaR. M Thorne - University of California, Los AngelesX Chu - University of California, Los AngelesL. G Ozeke - University of AlbertaG. D Reeves - Los Alamos National LaboratoryM. J Engebretson - Augsburg UniversityH. E Spence - University of New HampshireD. N Baker - University of Colorado BoulderJ. B Blake - The Aerospace CorporationJ. F Fennell - The Aerospace CorporationS. G Claudepierre - The Aerospace Corporation
- Resource Type
- Journal article
- Publication Details
- Journal of geophysical research. Space physics, Vol.123(3), pp.1938-1952
- DOI
- 10.1002/2017JA025114
- ISSN
- 2169-9380
- eISSN
- 2169-9402
- Number of pages
- 15
- Grant note
- NASA (NAS5‐01072; NNX15AI96G; NNX11AR64G; NNX14AN85G; NNX14AI18G; NNX17AD15G; NNX17AG07G) National Science Foundation (AGS 1451911; AGS‐1723588; PLR‐1341493; AGS‐1651263) AFOSR (FA9550‐15‐1‐0158) JHU/APL (967399; 921647)
- Language
- English
- Date published
- 03/2018
- Academic Unit
- Physics and Astronomy
- Record Identifier
- 9984199771502771
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