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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...
Wedi'i Gadw mewn:
| Prif Awduron: | , , |
|---|---|
| Fformat: | Artigo |
| Iaith: | Inglês |
| Cyhoeddwyd: |
Copernicus Publications
2000-04-01
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| Cyfres: | Annales Geophysicae |
| Mynediad Ar-lein: | https://www.ann-geophys.net/18/461/2000/angeo-18-461-2000.pdf |
| Tagiau: |
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