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Analysis of the positive ionospheric response to a moderate geomagnetic storm using a global numerical model
Current theories of <i>F</i>-layer storms are discussed using numerical simulations with the Upper Atmosphere Model, a global self-consistent, time dependent numerical model of the thermosphere-ionosphere-plasmasphere-magnetosphere system including electrodynamical coupling effects. A...
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| Huvudupphovsmän: | , , |
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| Materialtyp: | Artigo |
| Språk: | Inglês |
| Publicerad: |
Copernicus Publications
2000-04-01
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| Serie: | Annales Geophysicae |
| Länkar: | https://www.ann-geophys.net/18/461/2000/angeo-18-461-2000.pdf |
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