Modèle d'accrétion de glace sur un objet bidimensionnel fixe appliquable aux pales d'éoliennes by Guy Fortin, Adrian Ilinca, Jean-Louis Laforte

“…The roughness height depends on the surface water state, which can exist in the form of a film, bead or rivulet and is calculated from the equilibrium equation between the surface tension, aerodynamics and gravitational forces acting over the bead. …”
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