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Equivalent potential temperature

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Equivalent potential temperature, commonly referred to as Theta-e [\left( \theta_e \right)], is a measure of the instability of air at a given pressure, humidity, and temperature. Theta-e is the temperature of one parcel of air at 100 kPa (1000 mbar) after considering the energy from when the water vapor in the parcel is condensed.

Theoretically, it would be the temperature of the parcel if the following procedure were performed:

This resulting allows the comparison of parcels of air at different pressures, and is a measure of the instability of that air. [link]

The formula for theta-e is the following:[link]

[\theta_e = T_e \left( \frac \right)^\frac \approx \left( T + \frac } r \right) \left( \frac \right)^\frac ]

Where:

See also

Bibliography

Meteorological data and variables
Dew point | Heat index | Humidex | Wind chill | Water vapor | Atmospheric pressure | Temperature | Precipitation | Wind | Clouds | Lightning | Visibility | Convection | Theta-e | CAPE | CIN Sea surface temperature | Vorticity | Pot T | Humidity

External links

 


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