File:Upwelling3.jpeg

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Troisième étape de la formation d'un upwelling : La mer se rééquilibre, la couche chaude s'enfonce, les eaux froides remontent près des côtes.

Auteur : Nicolas Raymond

Date : 27 juillet 2005

Logiciel utilisé : Blender

Licence : Creative Commons avec obligation de mentionner l'auteur, les travaux dériver doivent utiliser une licence identique.

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current10:38, 13 December 2005Thumbnail for version as of 10:38, 13 December 2005640 × 480 (49 KB)Muu-karhu (talk | contribs){{CC-BY-SA}}

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