Affiliation:
1. State Key Laboratory of Space Weather National Space Science Center Chinese Academy of Sciences Beijing People's Republic of China
2. National Institute for Space Research (INPE) São José dos Campos Brazil
3. College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing People's Republic of China
Abstract
AbstractThe impact of upstream conditions on magnetopause reconnection has been an intriguing question in solar wind‐magnetosphere coupling. In this study, we conduct a statistical analysis of plasma properties in the reconnection outflow region and the associated upstream solar wind/magnetosheath. We observe that the normalized ion density (N/Nsw) decreases and the flow speed (V/Vsw) increases in the upstream magnetosheath with distance from the subsolar point, consistent with previous models and observations. The magnetic field strength (|B|), ion density (N), and ion bulk speed (|V|) in the upstream magnetosheath exhibit close correlations with those in the reconnection outflow region. This upstream‐downstream correlation likely arises from the process of forming reconnection outflows, where most upstream ions cross the separatrix and mix with ion outflow already accelerated near the X‐line. High‐speed part of reconnection outflow is mostly located on the magnetosphere side of the magnetopause current layer, with outflow velocities peaking close to the upstream magnetosheath Alfvén speed. The spatial extent of high‐speed outflow is greater in conditions of lower solar wind Alfvén Mach number (MA,sw). Additionally, the southward magnetic field in the magnetosheath and |B| of magnetopause current layer are larger in the cases of lower MA,sw. These findings indicate a close connection of plasma properties between the outflow region of magnetopause reconnection and the upstream magnetosheath.
Publisher
American Geophysical Union (AGU)
Cited by
1 articles.
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