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Keywords from Image Description:
Thorme de Sandstrm. fr Une masse d'eau de temprature initialement homogne est rchauffe une certaine profondeur d'un ct et refroidit de l'autre une profondeur diffrente Ceci engendre un phnomne de convection dans chaque zone et une circulation entre les deux zones Ainsi l'eau chauffe d'un ct s'lvera et l'eau froide de l'autre s'enfoncera