- Oct 22, 2014
- 22,758
Before going to sea, many sailors, fearing thunderstorms, check CAPE.
Why?
CAPE — Convective Available Potential Energy — reflects the presence in the atmosphere of a certain amount of energy that can be used for convection.
Convection is the rise of heated warmer air surrounded by cooler air. Warm air is lighter than cold air, so it is displaced upwards.
The more available energy that can be used for convection there is, the more intensive convection will be.
More intensive means faster and higher. High CAPE values indicate a high rate of convection development.
Here is a look at 2 regions with different CAPE index values.
The Puget Sound 0 J/kg

The Texas Coast 762 J/kg

Why?
CAPE — Convective Available Potential Energy — reflects the presence in the atmosphere of a certain amount of energy that can be used for convection.
Convection is the rise of heated warmer air surrounded by cooler air. Warm air is lighter than cold air, so it is displaced upwards.
The more available energy that can be used for convection there is, the more intensive convection will be.
More intensive means faster and higher. High CAPE values indicate a high rate of convection development.
Here is a look at 2 regions with different CAPE index values.
The Puget Sound 0 J/kg

The Texas Coast 762 J/kg
