Kelvin‐Helmholtz Waves and Magnetic Reconnection at the Earth's Magnetopause Under Southward Interplanetary Magnetic Field

Author:

Li Tongkuai12ORCID,Li Wenya13ORCID,Tang Binbin1ORCID,Khotyaintsev Yuri. V.4ORCID,Graham Daniel Bruce4ORCID,Ardakani Akhtar5,Burch J. L.6ORCID,Gershman D. J.78ORCID,Lavraud B.910ORCID,Russell C. T.11ORCID,Lu Quanming3ORCID,Guo Xiaocheng12ORCID,Wang Chi12ORCID

Affiliation:

1. State Key Laboratory of Space Weather National Space Science Center Chinese Academy of Sciences Beijing P. R. China

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

3. Key Laboratory of Geospace Environment University of Science and Technology of China Hefei P. R. China

4. Swedish Institute of Space Physics Uppsala Sweden

5. Institute for the Study of Earth, Oceans, and Space University of New Hampshire Durham NH USA

6. Southwest Research Institute San Antonio TX USA

7. NASA Goddard Space Flight Center Greenbelt MD USA

8. Department of Astronomy University of Maryland College Park MD USA

9. Laboratoire d’Astrophysique de Bordeaux University Bordeaux CNRS Pessac France

10. Institut de Recherche en Astrophysique et Planétologie Université de Toulouse CNRS UPS CNES Toulouse France

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

Abstract

AbstractWe present Magnetospheric Multiscale (MMS) observations of a K‐H wave event under southward IMF conditions, accompanied by ongoing magnetic reconnection. The nonlinear K‐H waves are characterized by quasi‐periodic fluctuations, the presence of low‐density and high‐speed ions, and variations in the boundary normal vectors at both the leading and trailing edges. Our observations reveal clear evidence of on‐going magnetic reconnection through the identification of Alfvénic ion jets and the escape of energetic magnetospheric electrons. Among the 36 magnetopause current‐sheet crossings in this event, 19 exhibit unambiguous signatures of reconnection at both the leading (7) and trailing (12) edges. Notably, the estimated current‐sheet thicknesses at both edges are comparable to the ion‐inertial scale, confirming the compression effect resulting from the large‐scale evolution of the K‐H waves. The reconnection jets potentially contribute to the suppression of K‐H growth through boundary‐layer broadening and the development of complex flow and magnetic field patterns.

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

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