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Also: EHI
At a glance
A simple product of CAPE × helicity that rolls 'enough energy' and 'enough spin' into one number. Higher is more tornadic.
Deep dive
EHI = (CAPE × SRH) / 160 000, using the 0–1 km (low-level EHI) or 0–3 km (deep EHI) layers.
Thresholds:
EHI is the ancestor of the STP; STP adds LCL height and bulk-shear terms and is generally preferred now. EHI still shows up in mesoanalysis displays because it's computationally cheap.