TY - JOUR
T1 - Particle‐in‐Cell Experiments Examine Electron Diffusion by Whistler‐Mode Waves
T2 - 2. Quasi‐Linear and Nonlinear Dynamics
AU - Allanson, Oliver
AU - Watt, Clare
AU - Ratcliffe, Heather
AU - Allison, Hayley
AU - Meredith, Nigel
AU - Bentley, Sarah
AU - Ross, John
AU - Glauert, Sarah
N1 - Funding Information:
The authors would like to thank the anonymous reviewers, whose comments have improved the manuscript. This research was supported by the Natural Environment Research Council (NERC) Highlight Topic Grants #NE/P017274/1 (Rad-Sat) and #NE/P01738X/1 (Rad-Sat), and also #NE/L002566/1. The research was also supported by STFC grants #ST/R505031/1 and #ST/R000921/1. This work was in part funded by the UK EPSRC grants EP/G054950/1, EP/G056803/1, EP/G055165/1 and EP/ M022463/1. This work was in part performed using the Cambridge Service for Data Driven Discovery (CSD3), part of which is operated by the University of Cambridge Research Computing on behalf of the STFC DiRAC HPC Facility (www.dirac.ac.uk). The DiRAC component of CSD3 was funded by BEIS capital funding via STFC capital grants ST/P002307/1 and ST/R002452/1 and STFC operations grant ST/R00689X/1. DiRAC is part of the National e-Infrastructure. This work was in part performed using the Reading Academic Computing Cluster (RACC) at the University of Reading. This work used the ARCHER UK National Supercomputing Service (http://www.archer.ac.uk).
Publisher Copyright:
©2020. The Authors.
Copyright:
Copyright 2020 Elsevier B.V., All rights reserved.
PY - 2020/7
Y1 - 2020/7
N2 - Test particle codes indicate that electron dynamics due to interactions with low amplitude incoherent whistler mode‐waves can be adequately described by quasi‐linear theory. However there is significant evidence indicating that higher amplitude waves cause electron dynamics not adequately described using quasi‐linear theory. Using the method that was introduced in Allanson et al. (2019, https://doi.org/10.1029/2019JA027088), we track the dynamical response of electrons due to interactions with incoherent whistler‐mode waves, across all energy and pitch angle space. We conduct five experiments each with different values of the electromagnetic wave amplitude. We find that the electron dynamics agree well with the quasi‐linear theory diffusion coefficients for low amplitude incoherent waves with (B w,rms/B 0)2≈3.7·10−10, over a time scale T of the order of 1,000 gyroperiods. However, the resonant interactions with higher amplitude waves cause significant nondiffusive dynamics as well as diffusive dynamics. When electron dynamics are extracted and analyzed over time scales shorter than T , we are able to isolate both the diffusive and nondiffusive (advective) dynamics. Interestingly, when considered over these appropriately shorter time scales (of the order of hundreds or tens of gyroperiods), the diffusive component of the dynamics agrees well with the predictions of quasi‐linear theory, even for wave amplitudes up to (B w,rms/B 0)2≈5.8·10−6. Quasi‐linear theory is based on fundamentally diffusive dynamics, but the evidence presented herein also indicates the existence of a distinct advective component. Therefore, the proper description of electron dynamics in response to wave‐particle interactions with higher amplitude whistler‐mode waves may require Fokker‐Planck equations that incorporate diffusive and advective terms.
AB - Test particle codes indicate that electron dynamics due to interactions with low amplitude incoherent whistler mode‐waves can be adequately described by quasi‐linear theory. However there is significant evidence indicating that higher amplitude waves cause electron dynamics not adequately described using quasi‐linear theory. Using the method that was introduced in Allanson et al. (2019, https://doi.org/10.1029/2019JA027088), we track the dynamical response of electrons due to interactions with incoherent whistler‐mode waves, across all energy and pitch angle space. We conduct five experiments each with different values of the electromagnetic wave amplitude. We find that the electron dynamics agree well with the quasi‐linear theory diffusion coefficients for low amplitude incoherent waves with (B w,rms/B 0)2≈3.7·10−10, over a time scale T of the order of 1,000 gyroperiods. However, the resonant interactions with higher amplitude waves cause significant nondiffusive dynamics as well as diffusive dynamics. When electron dynamics are extracted and analyzed over time scales shorter than T , we are able to isolate both the diffusive and nondiffusive (advective) dynamics. Interestingly, when considered over these appropriately shorter time scales (of the order of hundreds or tens of gyroperiods), the diffusive component of the dynamics agrees well with the predictions of quasi‐linear theory, even for wave amplitudes up to (B w,rms/B 0)2≈5.8·10−6. Quasi‐linear theory is based on fundamentally diffusive dynamics, but the evidence presented herein also indicates the existence of a distinct advective component. Therefore, the proper description of electron dynamics in response to wave‐particle interactions with higher amplitude whistler‐mode waves may require Fokker‐Planck equations that incorporate diffusive and advective terms.
KW - nonlinear theory
KW - particle-in-cell
KW - quasi-linear theory
KW - radiation belts
KW - wave-particle interaction
KW - whistler wave
UR - http://www.scopus.com/inward/record.url?scp=85088587434&partnerID=8YFLogxK
U2 - 10.1029/2020JA027949
DO - 10.1029/2020JA027949
M3 - Article
SN - 0148-0227
VL - 125
JO - Journal of Geophysical Research
JF - Journal of Geophysical Research
IS - 7
M1 - e2020JA027949
ER -