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.
Furthermore, adequate humidity combined with dew points in the 60s, convective available potential energy (CAPE) values in the 1,500–3,000 J/kg range, and very favorable low-level wind shear further destabilized the atmosphere, making it even more conducive to sustained supercells, capable of all hazards.