Characteristics of Rising Tone Whistler Mode Waves Inside the Earth's Plasmasphere, Plasmaspheric Plumes, and Plasmatrough-Reference-Cited by-同舟云学术

Characteristics of Rising Tone Whistler Mode Waves Inside the Earth's Plasmasphere, Plasmaspheric Plumes, and Plasmatrough

Published:2019-07 Issue:13 Volume:46 Page:7121-7130
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Teng S.¹²³^ORCID,Li W.³^ORCID,Tao X.¹²^ORCID,Shen X.‐C.³,Ma Q.³⁴^ORCID

Affiliation:

1. CAS Key Laboratory of Geospace Environment, Department of Geophysics and Planetary Sciences University of Science and Technology of China Hefei China

2. CAS Center for Excellence in Comparative Planetology Hefei China

3. Center for Space Physics Boston University Boston MA USA

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

Funder

National Natural Science Foundation of China

Alfred P. Sloan Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL083372

Reference72 articles.

1. Spatial Extent and Temporal Correlation of Chorus and Hiss: Statistical Results From Multipoint THEMIS Observations

2. Aspects of Nonlinear Wave-Particle Interactions

3. Oblique Whistler-Mode Waves in the Earth’s Inner Magnetosphere: Energy Distribution, Origins, and Role in Radiation Belt Dynamics

4. The nonlinear gyroresonance interaction between energetic electrons and coherent VLF waves propagating at an arbitrary angle with respect to the Earth's magnetic field

5. Nonlinear interaction of energetic electrons with large amplitude chorus

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