TY - JOUR
T1 - Particle‐in‐cell Experiments Examine Electron Diffusion by Whistler‐mode Waves
T2 - 1. Benchmarking With a Cold Plasma
AU - Allanson, Oliver
AU - Watt, Clare
AU - Ratcliffe, Heather
AU - Meredith, Nigel
AU - Allison, Hayley
AU - Bentley, Sarah
AU - Bloch, Teo
AU - Glauert, Sarah
PY - 2019/11
Y1 - 2019/11
N2 - Using a particle‐in‐cell code, we study the diffusive response of electrons due to wave‐particle interactions with whistler‐mode waves. The relatively simple configuration of field‐aligned waves in a cold plasma is used in order to benchmark our novel method, and to compare with previous works that used a different modelling technique. In this boundary‐value problem, incoherent whistler‐mode waves are excited at the domain boundary, and then propagate through the ambient plasma. Electron diffusion characteristics are directly extracted from particle data across all available energy and pitch‐angle space. The ‘nature’ of the diffusive response is itself a function of energy and pitch‐angle, such that the rate of diffusion is not always constant in time. However, after an initial transient phase, the rate of diffusion tends to a constant, in a manner that is consistent with the assumptions of quasilinear diffusion theory. This work establishes a framework for future investigations on the nature of diffusion due to whistler‐mode wave‐particle interactions, using particle‐in‐cell numerical codes with driven waves as boundary value problems.
AB - Using a particle‐in‐cell code, we study the diffusive response of electrons due to wave‐particle interactions with whistler‐mode waves. The relatively simple configuration of field‐aligned waves in a cold plasma is used in order to benchmark our novel method, and to compare with previous works that used a different modelling technique. In this boundary‐value problem, incoherent whistler‐mode waves are excited at the domain boundary, and then propagate through the ambient plasma. Electron diffusion characteristics are directly extracted from particle data across all available energy and pitch‐angle space. The ‘nature’ of the diffusive response is itself a function of energy and pitch‐angle, such that the rate of diffusion is not always constant in time. However, after an initial transient phase, the rate of diffusion tends to a constant, in a manner that is consistent with the assumptions of quasilinear diffusion theory. This work establishes a framework for future investigations on the nature of diffusion due to whistler‐mode wave‐particle interactions, using particle‐in‐cell numerical codes with driven waves as boundary value problems.
KW - Radiation belt
KW - Wave‐particle interaction
KW - Whistler‐mode wave
KW - Particle‐in‐cell
KW - Numerical experiment
KW - Quasilinear theory
U2 - 10.1029/2019JA027088
DO - 10.1029/2019JA027088
M3 - Article
VL - 124
SP - 8893
EP - 8912
JO - Journal of Geophysical Research: Oceans
JF - Journal of Geophysical Research: Oceans
SN - 2169-8953
IS - 11
ER -