Abstract
Reconnection is the key process responsible for the magnetotail dynamics. Driven reconnection in the distant tail is not sufficient to support global magnetospheric convection and the near Earth neutral line spontaneously forms to restore the balance. Mechanisms of initiation of such near-Earth magnetotail reconnection still represent one of major unresolved issues in space physics. We review the progress in this topic during the last decade. Recent theoretical advances suggest several variants of overcoming the famous tearing stability problem. Multipoint spacecraft observations reveal detailed structure of pre-onset current sheet of and reconnection zone down to ion larmor scale, supporting the importance of unstable state development through internal magnetotail reconfiguration.
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Acknowledgements
The authors thank Waileong Teh and Rongsheng Wang for the use of figures they made and/or assisted with. Authors would like to acknowledge Cluster Science Archive and Cluster instrument teams, in particular FGM, CIS, PEACE, EFW for excellent data.
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Petrukovich, A., Artemyev, A., Nakamura, R. (2016). Magnetotail Reconnection. In: Gonzalez, W., Parker, E. (eds) Magnetic Reconnection. Astrophysics and Space Science Library, vol 427. Springer, Cham. https://doi.org/10.1007/978-3-319-26432-5_7
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