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Ion precipitation in the cusp for northward IMF and its relationship with magnetosheath flow

Abstract If the interplanetary magnetic field (IMF) has a northward component, a portion of the solar wind ions flowing in the high-latitude magnetosheath drastically alters the flow direction owing to lobe reconnection and follows the Earth's magnetic field lines toward the low-altitude cusp. Partl...

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Autors principals: Haruto Koike, Satoshi Taguchi
Format: Artigo
Idioma:Inglês
Publicat: SpringerOpen 2024-05-01
Col·lecció:Earth, Planets and Space
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Accés en línia:https://doi.org/10.1186/s40623-024-02011-w
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