File:Transport Ekman.png
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editDescriptionTransport Ekman.png |
Français : Transport horizontal et vertical de l'eau dans l'océan à cause de la force de Coriolis qui produit la Spirale d'Ekman. Dans une dépression, les vents tournant de façon anti-horaire, le force de Coriolis dévie l'eau vers l'extérieur ce qui crée un déficit au centre du système et un Pompage vertical. L'inverse se produit dans le cas d'un anticyclone. |
Date | (UTC) |
Source | Own work |
Author | Pierre cb |
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Date/Time | Thumbnail | Dimensions | User | Comment | |
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current | 12:09, 2 October 2016 | ![]() | 971 × 394 (68 KB) | Cmdrjameson (talk | contribs) | Compressed with pngout. Reduced by 40kB (37% decrease). |
15:10, 18 November 2006 | ![]() | 971 × 394 (108 KB) | Pierre cb (talk | contribs) | Transport horizontal et vertical de l'eau dans l'océan à cause de la force de Coriolis qui produit la Spirale d'Ekman. Dans une dépression, les vents tournant de façon anti-horaire, le force de Coriolis dévie l'eau vers l'extérieur ce qui crée un d |
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