Logo image
A radio oval above Earth’s auroral oval
Journal article   Open access   Peer reviewed

A radio oval above Earth’s auroral oval

Siyuan Wu, Daniel K. Whiter, Laurent Lamy, Ulrich Taubenschuss, Philippe Zarka, Brieuc Collet, Xiangyu Wang, Georg Fischer, Hao Ning, Yao Chen, …
Science advances, Vol.12(13), eaec4114
03/27/2026
DOI: 10.1126/sciadv.aec4114
PMID: 41894503
url
https://doi.org/10.1126/sciadv.aec4114View
Published (Version of record) Open Access

Abstract

Auroral kilometric radiation (AKR), Earth’s strongest radio emission, has long been associated with discrete auroras and electrons near a few kilo–electron volt (keV) range. However, auroras also occur in diffuse forms with broader electron energies, raising the question of why AKR has not been observed above diffuse auroras or linked to electrons outside the kilo–electron volt population. Comprehensive AKR source distributions have remained elusive because of observational limitations, and their local-time coverage remains largely unknown. Using spacecraft measurements, we identify a “radio oval” above the optical auroral oval, spanning the full local-time range, where AKR is emitted over both discrete and diffuse auroras. The AKR source electrons display diverse precipitation features, including monoenergetic (peak flux at 3.82 kilo–electron volts), broadband (1.34 kilo–electron volts), low-energy (0.47 kilo–electron volts), and diffuse types (>1 kilo–electron volt). These results reveal that the cyclotron maser instability—the mechanism driving AKR—can arise in diverse plasma environments, broadening our understanding of both AKR generation and auroral complexity. Radio waves called AKR radiate above auroras, driven by diverse electron acceleration and precipitation processes.
Astronomy Geophysics Earth, Environmental, Ecological, and Space Sciences SciAdv r-articles

Details

Logo image