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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...

Täydet tiedot

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Bibliografiset tiedot
Päätekijä: Naohiko Hirasawa
Aineistotyyppi: Artigo
Kieli:Inglês
Julkaistu: National Institute of Polar Research 2010-12-01
Sarja:Antarctic Record
Linkit:http://doi.org/10.15094/00009559
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