Nonresonant Scattering of Energetic Electrons by Electromagnetic Ion Cyclotron Waves: Spacecraft Observations and Theoretical Framework

Author:

An Xin1ORCID,Artemyev Anton1ORCID,Angelopoulos Vassilis1ORCID,Zhang Xiao‐Jia2ORCID,Mourenas Didier34,Bortnik Jacob5ORCID,Shi Xiaofei1ORCID

Affiliation:

1. Department of Earth, Planetary, and Space Sciences University of California Los Angeles Los Angeles CA USA

2. Department of Physics University of Texas at Dallas Richardson TX USA

3. CEA DAM DIF Arpajon France

4. Laboratoire Matière en Conditions Extrêmes Paris‐Saclay University CEA Bruyères‐le‐Châtel France

5. Department of Atmospheric and Oceanic Sciences University of California Los Angeles Los Angeles CA USA

Abstract

AbstractElectromagnetic ion cyclotron (EMIC) waves lead to rapid scattering of relativistic electrons in Earth's radiation belts, due to their large amplitudes relative to other waves that interact with electrons of this energy range. A central feature of electron precipitation driven by EMIC waves is deeply elusive. That is, moderate precipitating fluxes at energies below the minimum resonance energy of EMIC waves occur concurrently with strong precipitating fluxes at resonance energies in low‐altitude spacecraft observations. This paper expands on a previously reported solution to this problem: nonresonant scattering due to wave packets. The quasi‐linear diffusion model is generalized to incorporate nonresonant scattering by a generic wave shape. The diffusion rate decays exponentially away from the resonance, where shorter packets lower decay rates and thus widen the energy range of significant scattering. Using realistic EMIC wave packets from δf particle‐in‐cell simulations, test particle simulations are performed to demonstrate that intense, short packets extend the energy of significant scattering well below the minimum resonance energy, consistent with our theoretical prediction. Finally, the calculated precipitating‐to‐trapped flux ratio of relativistic electrons is compared to ELFIN observations, and the wave power spectra is inferred based on the measured flux ratio. We demonstrate that even with a narrow wave spectrum, short EMIC wave packets can provide moderately intense precipitating fluxes well below the minimum resonance energy.

Funder

National Science Foundation

National Aeronautics and Space Administration

Publisher

American Geophysical Union (AGU)

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