View source for Convective Available Potential Energy

== Introduction ==
Convective Available Potential Energy (CAPE) is a measure of the amount of energy available for convection. Convection is the process by which heat is transferred by the mass movement of a fluid, such as air or water. CAPE is directly related to the potential severity of convective weather phenomena such as thunderstorms, and is used in meteorology to predict the development of such phenomena.

== Definition and Calculation ==
CAPE is defined as the total amount of kinetic energy that a parcel of air would have if it were lifted a certain distance vertically through the atmosphere. It is usually measured in joules per kilogram (J/kg). The calculation of CAPE involves the integration of the area on a thermodynamic diagram (such as a [[Skew-T log-P diagram]]) between the environmental temperature profile and the path of a rising air parcel, over the layer within which the parcel is warmer than the environment.

== Importance in Meteorology ==
In meteorology, CAPE is a vital parameter for the prediction of severe weather. High values of CAPE are associated with severe convective storms, including thunderstorms, hailstorms, and tornadoes. CAPE is also used in the prediction of other weather phenomena such as heavy rainfall and flash floods.

== Factors Influencing CAPE ==
Several factors can influence the amount of CAPE in the atmosphere. These include the lapse rate (the rate at which temperature decreases with height), the moisture content of the air, and the temperature of the air at the surface. A steep lapse rate, high moisture content, and high surface temperature can all contribute to high CAPE values.

== Measurement and Analysis ==
CAPE is typically measured using radiosondes, which are instruments attached to weather balloons that measure various atmospheric parameters as they ascend through the atmosphere. The data obtained from radiosondes is then used to construct a thermodynamic diagram, which is analyzed to calculate CAPE.

== Applications ==
Beyond weather forecasting, CAPE is also used in climate studies to understand the dynamics of the atmosphere and its response to changes in temperature and moisture content. It is also used in the study of air pollution, as it can influence the dispersion of pollutants in the atmosphere.

== Limitations ==
While CAPE is a useful parameter for predicting severe weather, it has its limitations. For instance, it does not take into account the effects of wind shear, which can significantly influence the development and severity of convective storms. Furthermore, high CAPE values do not guarantee the occurrence of severe weather, as other factors such as atmospheric stability and triggering mechanisms for convection also play a role.

== See Also ==
* [[Atmospheric convection]]
* [[Severe weather]]
* [[Weather forecasting]]
* [[Climate studies]]
* [[Air pollution]]

[[Image:Detail-58786.jpg|thumb|center|A photograph of a thunderstorm developing in an atmosphere with high CAPE.|class=only_on_mobile]]
[[Image:Detail-58787.jpg|thumb|center|A photograph of a thunderstorm developing in an atmosphere with high CAPE.|class=only_on_desktop]]

[[Category:Meteorology]]
[[Category:Weather forecasting]]
[[Category:Atmospheric physics]]