NEWeatherguy wrote:Mike, I found the following at SPC's website:
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MUCAPE (Most Unstable Convective Available Potential Energy) is a measure of instability in the troposphere. This value represents the total amount of potential energy available to the most unstable parcel of air found within the lowest 300-mb of the atmosphere while being lifted to its level of free convection (LFC). No parcel entrainment is considered. The CAPE calculation uses virtual temperatures, but the CIN value does not. SPC forecasters have noted that non-virtual CIN calculations tend to define areas of weak cap more accurately than if the virtual temperature was considered.
That pretty much covers the background info on MUCAPE, but there is a critical thing left out in the SPC description.
Like the best LI (lifted index), MUCAPE is best suited for use when dealing with a shallow cool (or relatively stable) layer close to the boundary layer, which would make surface based CAPE values unrepresentative of the instability present above the shallow stable layer. the same thing goes for surface based LI values.
similarly, the Showalter index is fairly useful when dealing with low level stability.