Statistical Analysis of Whistler Precursors Upstream of Foreshock Transient Shocks: MMS Observations

Author:

Wang Mengmeng12ORCID,Liu Terry Z.3ORCID,Zhang Hui1ORCID,Liu Kaijun2ORCID,Shi Quanqi1ORCID,Guo Ruilong1ORCID,Tian Anmin1ORCID,Sun Weijie4ORCID,Shen Xiao‐Chen5ORCID,Wu Siyuan26ORCID,Degeling Alexander W.1ORCID,Wang Yan2ORCID,Bai Shi‐Chen17ORCID,Yao Zhonghua8ORCID,Li Wenya9ORCID,Zhang Shuai2ORCID,Pitkänen Timo110ORCID,Yao Shutao1ORCID,Liu Ji11,Cheng Kun2,Ma Xiao1ORCID,Liu Yuqi2ORCID

Affiliation:

1. Shandong Provincial Key Laboratory of Optical Astronomy and Solar‐Terrestrial Environment Institute of Space Sciences Shandong University Weihai China

2. Department of Earth and Space Sciences Southern University of Science and Technology Shenzhen China

3. Department of Earth, Planetary, and Space Sciences University of California, Los Angeles Los Angeles CA USA

4. Space Sciences Laboratory University of California, Berkeley Berkeley CA USA

5. Center for Space Physics Boston University Boston MA USA

6. LESIA Observatoire de Paris CNRS Université PSL Sorbonne Université Université Paris Cité CNRS Meudon France

7. School of Mathematics and Statistics Shandong University Weihai China

8. Department of Earth Sciences The University of Hong Kong Hong Kong China

9. State Key Laboratory of Space Weather National Space Science Center Chinese Academy of Sciences Beijing China

10. Department of Physics Umeå University Umeå Sweden

11. Department of Physics University of Alberta Edmonton AB Canada

Abstract

AbstractUsing the high‐time‐resolution data from the Magnetospheric Multiscale mission, precursor waves upstream of foreshock transient (FT) shocks are statistically investigated using the four‐spacecraft timing method. The wave frequencies and wave vectors determined in the plasma rest frame (PRF) are shown to follow the cold plasma dispersion relation for whistler waves. Combining with the feature of the right‐hand polarization in the PRF, the precursors are identified as whistler‐mode waves around the lower hybrid frequency. The occurrence of whistler precursors is independent of the Alfvén Mach number and the FT shock normal angle. More importantly, all the whistler precursors have group velocities pointing upstream in the shock frame, suggesting the dispersive radiation to be a possible generation mechanism. The study improves the understanding of not only the whistler precursors but also the overall FT shock dynamics.

Publisher

American Geophysical Union (AGU)

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