CAS Key Laboratory of Geospace Environment, Department of Engineering and Applied Physics, University of Science and Technology of China, Hefei, Anhui, China
KTX Laboratory, Department of Engineering and Applied Physics, University of Science and Technology of China, Hefei, Anhui, China
Department of Engineering Physics, University of Wisconsin-Madison, Madison, Wisconsin, USA
now at: Huazhong University of Science and Technology, Wuhan, Hubei 430074, China
Zechen Wang
CAS Key Laboratory of Geospace Environment, Department of Engineering and Applied Physics, University of Science and Technology of China, Hefei, Anhui, China
Jun Chen
CAS Key Laboratory of Geospace Environment, Department of Geophysics and Planetary Sciences, University of Science and Technology of China, Hefei, Anhui, China
Xingting Yan
CAS Key Laboratory of Geospace Environment, Department of Engineering and Applied Physics, University of Science and Technology of China, Hefei, Anhui, China
CAS Key Laboratory of Geospace Environment, Department of Geophysics and Planetary Sciences, University of Science and Technology of China, Hefei, Anhui, China
CAS Center for Excellence in Comparative Planetology, Hefei, Anhui, China
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Total article views: 2,927 (including HTML, PDF, and XML)
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Total article views: 2,234 (including HTML, PDF, and XML)
Thereof 2,234 with geography defined
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Total article views: 693 (including HTML, PDF, and XML)
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Our research explores a new method for identifying where and when the magnetic field lines in Earth's magnetotail may change its topology through the reconnection process, during which a sudden release of magnetic energy can lead to the brightening of aurora, a process called substorm. Traditionally, the magnetic reconnection was often interpreted using a two-dimensional model, which however does not capture the intrinsically three-dimensional nature of reconnection physics, as we have revealed.
Our research explores a new method for identifying where and when the magnetic field lines in...