File:Transport Ekman.png
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Size of this preview: 800 × 325 pixels. Other resolutions: 320 × 130 pixels | 971 × 394 pixels.
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[edit]DescriptionTransport 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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[edit]I, the copyright holder of this work, hereby publish it under the following licenses:
Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License.http://www.gnu.org/copyleft/fdl.htmlGFDLGNU Free Documentation Licensetruetrue |
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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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