Whistler‐Mode Waves Inside Short Large‐Amplitude Magnetic Field Structures: Characteristics and Generation Mechanisms

Author:

Bai Shi‐Chen123ORCID,Shi Quanqi2ORCID,Shen Xiao‐Chen4ORCID,Tian Anmin23ORCID,Zhang Hui2ORCID,Guo Ruilong2ORCID,Wang Mengmeng25ORCID,Degeling Alexander W.2ORCID,Bu Yude1,Zhang Shuai5ORCID,Ma Xiao2ORCID

Affiliation:

1. School of Mathematics and Statistics Shandong University Weihai China

2. Shandong Provincial Key Laboratory of Optical Astronomy and Solar‐Terrestrial Environment Institute of Space Sciences Shandong University Weihai People's Republic of China

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

4. Center for Space Physics Boston University Boston MA USA

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

Abstract

AbstractShort large‐amplitude magnetic structures (SLAMS) frequently appear near the bow shock. Inside steepening SLAMS, whistler‐mode waves are coherently generated at their leading edges. These waves are crucial for electron dynamics, energy conversion and magnetic reconnection near the shock. Nevertheless, the characteristics and generation of the whistler‐mode waves inside SLAMS are still unclear. In this study, we conducted a statistical analysis of whistler‐mode waves within SLAMS near the Earth's bow shock to investigate their properties and generation mechanisms. We found that these waves are mainly excited by electron temperature anisotropy with 99% of them falling below the nonlinear resonant threshold. The combination of a low background magnetic field and intense steepening at SLAMS' leading edge makes it the main source region of whistler‐mode waves and may induce the nonlinear resonance of whistler‐mode waves.

Funder

National Natural Science Foundation of China

Macau University of Science and Technology

Publisher

American Geophysical Union (AGU)

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