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Winter warming-event observed at Dome Fuji Station and synoptic-scale circulation in the Antarctic
The atmosphere over the Antarctic interior is usually separated from the outside by circumpolar tight potential vorticity gradients, where surface transient eddies are embedded, at the Dome Fuji Station (77゜S, 40゜E) on the topographical ridge of the East Antarctic ice sheet, an intensive meteorologi...
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| Autor principal: | |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Institute of Polar Research
2010-12-01
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| Colecção: | Antarctic Record |
| Acesso em linha: | http://doi.org/10.15094/00009559 |
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