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Right-moving supercells (highly-organised mesocyclonic thunderstorms with cyclonic flow at the mesoscale) developed over NE Spain producing giant hail and floods in Zaragoza. Large deep-layer shear (over 30 m s-1 0-6 km shear) coexisted with a quite large MUCAPE. ENS mostly about 1500J kg-1 with extreme above 2000 J kg-1. Very low values of convective inhibition (CIN) in the moist air in the lowest layers and the level of free convection (LFC) and lifted condensation level (LCL) were strong signals for the very active convection.
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