Abstract
Particle-in-cell simulations were performed to understand the interaction of the
solar wind with localized magnetic fields on the sunlit surface of the Moon. The results
indicated a mini-magnetosphere was formed which had a thin magnetopause with the
thickness of the electron skin depth. It was also found that the solar wind penetrated
into the cavity of the magnetosphere intermittently rather than in a steady manner. The
solar wind that moved around the magnetosphere was observed to hit the surface of the
Moon, implying that it may be the cause of the lunar swirl formation on the surface.
Publisher
The Korean Space Science Society
Subject
General Earth and Planetary Sciences,General Physics and Astronomy
Cited by
1 articles.
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