Ion Acceleration and Corresponding Bounce Echoes Induced by Electric Field Impulses: MMS Observations

Author:

Li Xing‐Yu1ORCID,Liu Zhi‐Yang1ORCID,Zong Qiu‐Gang12ORCID,Zhou Xu‐Zhi1ORCID,Liu Jian‐Jun3ORCID,Hu Ze‐Jun3ORCID,Zhao Xing‐Xin13ORCID,Hao Yi‐Xin4ORCID,Liu Ying1ORCID,Yang Fan1ORCID,Pollock Craig J.5ORCID,Russell Christopher T.6ORCID,Lindqvist Per‐Arne7ORCID

Affiliation:

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

2. State Key Laboratory of Lunar and Planetary Sciences Macau University of Science and Technology Taipa China

3. MNR Key Laboratory for Polar Science Polar Research Institute of China Shanghai China

4. Max Planck Institute for Solar System Research Göttingen Germany

5. Denali Scientific Fairbanks AK USA

6. Department of Earth and Space Sciences University of California Los Angeles CA USA

7. Department of Space and Plasma Physics KTH Royal Institute of Technology Stockholm Sweden

Abstract

AbstractDayside magnetosphere interactions are essential for energy and momentum transport between the solar wind and the magnetosphere. In this study, we investigate a new phenomenon within this regime. Sudden enhancements of ion fluxes followed by repeating dropouts and recoveries were observed by Magnetospheric Multiscale on 5 November 2016, which is the very end of the recovery phase from a moderate geomagnetic storm. These repetitive flux variations display energy‐dispersive characteristics with periods relevant to ion bounce motion, suggesting they are corresponding echoes. Alongside the flux variations, bipolar electric field impulses originating from external sources were detected. We traced the source region of the initial injection and found it is located near the spacecraft's position. To elucidate the underlying physics, a test‐particle simulation is conducted. The results reveal that radial transport resulting from impulse‐induced acceleration can give rise to these echoes. Observations demonstrate dayside magnetosphere interactions are more common than we previously considered, which warrants further research.

Publisher

American Geophysical Union (AGU)

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