On the possibility of ion-drag to induce dynamic instability in the lower thermosphere neutral gas
Strong wind shears may result in dynamic instability, often characterised by the Richardson number lying between zero and 0.25. The extent to which electric-field driven ion flow may induce such neutral wind shears is examined. Further, it is proposed that, in the ionosphere, it is possible for...
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| Autor principal: | |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Copernicus Publications
2000-08-01
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| coleção: | Annales Geophysicae |
| Acesso em linha: | https://www.ann-geophys.net/18/967/2000/angeo-18-967-2000.pdf |
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