MESSENGER Observations of Reconnection in Mercury's Magnetotail Under Strong IMF Forcing

Author:

Zhong Jun12ORCID,Lee Lou‐Chuang34ORCID,Slavin James A.5ORCID,Zhang Hui12ORCID,Wei Yong12ORCID

Affiliation:

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

2. Heilongjiang Mohe National Observatory of Geophysics Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China

3. Institute of Earth Sciences Academia Sinica Taipei Taiwan

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

5. Department of Climate and Space Sciences and Engineering University of Michigan Ann Arbor MI USA

Abstract

AbstractThe MESSENGER spacecraft typically crossed Mercury's magnetotail current sheet relatively close to the planet, that is, less than 2.5 RM (planet radius; 2,440 km). Magnetometer measurements are used to detect active reconnection events by identifying the quadrupole Hall magnetic field signatures that form about X‐lines. Statistical analyses of the 51 active reconnection events detected in this manner indicate that they occur most frequently on the duskside and typically at a mean altitude greater than 1.5 RM. In contrast, the dawnside events occur at altitudes of ∼1 RM. In addition, a higher recurrence rate of flux ropes formed in the Hall region was observed on the dawnside. Applying the Kan‐Lee solar wind‐magnetosphere coupling function confirmed that these near‐tail reconnection events at Mercury are observed under strong forcing by the interplanetary magnetic field. We further propose that the reconnection‐driven nightside magnetosphere‐planet interaction is characterized by a pronounced dawn‐dusk asymmetry and may significantly influence the near‐Mercury space environment.

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Geophysics

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