1. What is CAP?

The CAP is a stable region of the lower troposphere that impedes convection in the PBL from occurring.

2. How is CAP determined?

The CAP is determined as the maximum temperature difference between a parcel of air and the surrounding actual temperature in the lower troposphere.

Formula: Environmental temperature - parcel temperature (both in region with max temperature difference)

The CAP will always be a positive number since a CAP region has a parcel temperature that is colder than the surrounding environment. CAP is given in units of Celsius difference. This temperature difference is the amount of warming (or rather the weather conditions that will cause the parcel to no longer be colder than surrounding environment) required to produce no CAP.

The CAP on the sounding at the bottom is 1.1 (weak for a morning sounding CAP).

3. Operational significance of CAP:

0 No Cap
0.1 - 1.9 Weak Cap
2.0 - 4.0 Moderate Cap
4.1+ Strong Cap

When the CAP is less than 2.0, storms are likely to develop shortly when the only parameter holding back convection is the CAP.

When the CAP is greater than 4, help will be needed over the next few hours to break it.

4. Pitfalls:

a. Pay attention to factors that can rapidly weaken a cap: synoptic uplift, daytime heating, low level convergence

b. Does not consider elevated convection; CAP is a warm season- warm sector index

c. Index is meaningless if there is zero CAPE in troposphere