Boundary layer interaction in plume-based variable-viscosity thermal convection

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Résumé : Nous avons mesuré la fréquence de formation de panaches dans une expérience de convection thermique à Pr >>1. Comme la viscosité du fluide utilisé varie fortement avec la température, les couches limites chaude et froide ont différentes épaisseurs et viscosités. Ceci entraîne des fréquences différentes pour ces couches. Il semblerait qu’il y ait une interaction directe entre les couches limites, par l’intermédiaire des panaches. En particulier, s’il y a une fréquence principale bien définie pour l’apparition de panaches froids, il y a en a plusieurs pour les panaches chauds, dont l’une est celle des panaches froids. Ces mesures suggèrent donc que des « panaches » froids dans le manteau (les pans de croûte plongeant dans les zones de subduction) peuvent indure des panaches chauds.

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تاریخ انتشار 2007