Whistler-mode chorus waves at Mars.


Journal

Nature communications
ISSN: 2041-1723
Titre abrégé: Nat Commun
Pays: England
ID NLM: 101528555

Informations de publication

Date de publication:
06 Jun 2023
Historique:
received: 28 07 2022
accepted: 11 05 2023
medline: 7 6 2023
pubmed: 7 6 2023
entrez: 6 6 2023
Statut: epublish

Résumé

Chorus waves are naturally occurring electromagnetic emissions in space and are known to produce highly energetic electrons in the hazardous radiation belt. The characteristic feature of chorus is its fast frequency chirping, whose mechanism remains a long-standing problem. While many theories agree on its nonlinear nature, they differ on whether or how the background magnetic field inhomogeneity plays a key role. Here, using observations of chorus at Mars and Earth, we report direct evidence showing that the chorus chirping rate is consistently related to the background magnetic field inhomogeneity, despite orders of magnitude difference in a key parameter quantifying the inhomogeneity at the two planets. Our results show an extreme test of a recently proposed chorus generation model and confirm the connection between the chirping rate and magnetic field inhomogeneity, opening the door to controlled plasma wave excitation in the laboratory and space.

Identifiants

pubmed: 37280247
doi: 10.1038/s41467-023-38776-z
pii: 10.1038/s41467-023-38776-z
pmc: PMC10244391
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

3142

Subventions

Organisme : National Natural Science Foundation of China (National Science Foundation of China)
ID : 42174182
Organisme : National Natural Science Foundation of China (National Science Foundation of China)
ID : 11235009

Informations de copyright

© 2023. The Author(s).

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Auteurs

Shangchun Teng (S)

Deep Space Exploration Laboratory/School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China.
CAS Center for Excellence in Comparative Planetology/CAS Key Laboratory of Geospace Environment, University of Science and Technology of China, Hefei, China.
State Key Laboratory of Marine Geology, School of Ocean and Earth Science, Tongji University, Shanghai, China.

Yifan Wu (Y)

Deep Space Exploration Laboratory/School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China.
CAS Center for Excellence in Comparative Planetology/CAS Key Laboratory of Geospace Environment, University of Science and Technology of China, Hefei, China.

Yuki Harada (Y)

Department of Geophysics, Kyoto University, Kyoto, Japan.

Jacob Bortnik (J)

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

Fulvio Zonca (F)

Center for Nonlinear Plasma Science and C.R. ENEA Frascati, Frascati, Italy.
Institute of Fusion Theory and Simulation and School of Physics, Zhejiang University, Hangzhou, China.

Liu Chen (L)

Institute of Fusion Theory and Simulation and School of Physics, Zhejiang University, Hangzhou, China.
Department of Physics and Astronomy, University of California, Irvine, USA.

Xin Tao (X)

Deep Space Exploration Laboratory/School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China. xtao@ustc.edu.cn.
CAS Center for Excellence in Comparative Planetology/CAS Key Laboratory of Geospace Environment, University of Science and Technology of China, Hefei, China. xtao@ustc.edu.cn.

Classifications MeSH