Additionally, sufficient moisture aided by dew points in the 60s, convective available potential energy (CAPE) values in the 1,500–3000 J/kg range, and very favorable low-level wind shear further destabilized the atmosphere, making it even more favorable for sustained supercells, capable of all hazards.
In this context, sufficient moisture combined with dew points in the 60s, convective available potential energy (CAPE) values between 1,500–3,000 J/kg, and very favorable low-level wind shear further destabilized the atmosphere, creating a highly favorable condition for sustained supercells that can pose all types of hazards.