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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| Asıl Yazarlar: | , |
|---|---|
| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
SpringerOpen
2024-05-01
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| Seri Bilgileri: | Earth, Planets and Space |
| Konular: | |
| Online Erişim: | https://doi.org/10.1186/s40623-024-02011-w |
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