Bursty Energetic Electron Precipitation by High‐Order Resonance With Very‐Oblique Whistler‐Mode Waves

Author:

Gan Longzhi1ORCID,Artemyev Anton2ORCID,Li Wen1ORCID,Zhang Xiao‐Jia23ORCID,Ma Qianli14ORCID,Mourenas Didier56,Angelopoulos Vassilis2ORCID,Tsai Ethan2ORCID,Wilkins Colin2ORCID

Affiliation:

1. Center for Space Physics Boston University Boston MA USA

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

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

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

5. CEA DAM DIF Arpajon France

6. Laboratoire Mati`ere en Conditions Extrˆemes Paris‐Saclay University CEA Bruy`eres‐le‐Chˆatel France

Abstract

AbstractResonant interactions with whistler‐mode waves are one of the most important drivers for rapid energetic electron precipitation. In this letter, we study a conjunction event, where bursts of energetic electron precipitation (50–800 keV) with timescales of several seconds are observed by the twin ELFIN Cubesats at low Earth orbit, while very‐oblique intense whistler‐mode waves are observed by the Time History of Events and Macroscale Interactions during Substorms E satellite at the conjugate magnetic equator. Our observation‐constrained test‐particle simulations reveal that the electron precipitation, particularly above 100 keV, results from high‐order resonant scattering by the very‐oblique whistler‐mode waves. Our study provides the first direct evidence for high‐order resonance driven precipitation, explaining a bursty precipitation event. The results demonstrate that high‐order resonant scattering could be important, not only in long‐term diffusion models, but also in models of short timescale events.

Funder

National Science Foundation

National Aeronautics and Space Administration

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

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