A Radial Standing Pc5‐6 Wave and Its Energy Coupling With Field Line Resonance Within the Dusk‐Sector Magnetosphere

Author:

Zhou Yi‐Jia12ORCID,He Fei12ORCID,Zhang Xiao‐Xin3,Archer Martin O.4ORCID,Lin Yu5ORCID,Ma Han12ORCID,Tian An‐Min6ORCID,Yao Zhong‐Hua12ORCID,Wei Yong12,Ni Binbin7ORCID,Liu Wenlong8ORCID,Zong Qiu‐Gang9ORCID,Pu Zu‐Yin9ORCID

Affiliation:

1. Key Laboratory of Earth and Planetary Physics Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China

2. College of Earth and Planetary Science University of Chinese Academy of Sciences Beijing China

3. Key Laboratory of Space Weather National Center for Space Weather China Meteorological Administration Beijing China

4. Space and Atmospheric Physics Group Department of Physics Imperial College London London UK

5. Physics Department Auburn University Auburn AL USA

6. School of Space Science and Physics Shandong University Weihai China

7. Department of Space Physics School of Electronic Information Wuhan University Wuhan China

8. School of Space and Environment Beihang University Beijing China

9. Institute of Space Physics and Applied Technology Peking University Beijing China

Abstract

AbstractGlobal ultra‐low frequency (ULF) oscillations are believed to play a significant role in the mass, energy, and momentum transport within the Earth's magnetosphere. In this letter, we observe a ∼1.2 mHz radial standing wave in the dusk‐sector magnetosphere accompanied by the field line resonance (FLR) on 16 July 2017. The frequency estimation from the simple box model also confirms the radial standing wave. The essential characteristics of FLR are concurrently identified at the dusk‐sector magnetosphere and the conjugated ground location. Further, the radial standing wave dissipates energy into upper atmosphere to enhance the local aurora by coupling itself to the FLR. The magnetospheric dominant 1.2/1.1 mHz ULF waves plausibly correspond well with the discrete ∼1 mHz magnetosheath ion dynamic pressure/velocity oscillation, suggesting this radial standing wave and FLR in the flank magnetosphere may be triggered by the solar‐wind and/or magnetosheath dynamic pressure/velocity fluctuations.

Funder

National Natural Science Foundation of China

National Key Research and Development Program of China

Youth Innovation Promotion Association of the Chinese Academy of Sciences

Institute of Geology and Geophysics, Chinese Academy of Sciences

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Geophysics

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