Wet-bulb potential temperature
Type of temperature measurement
Wet-bulb potential temperature, sometimes referred to as pseudo wet-bulb potential temperature, is the temperature that a parcel of air at any level would have if, starting at the wet-bulb temperature, it were brought at the saturated adiabatic lapse rate to the standard pressure of 1,000 mbar.
This temperature is conservative with respect to reversible adiabatic changes.
See also
- Wet-bulb temperature
- Potential temperature
- Atmospheric thermodynamics
- Equivalent temperature
- Equivalent potential temperature
External links
- AMS Glossary
- Oxford Index
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Meteorological data and variables
- Adiabatic processes
- Advection
- Buoyancy
- Lapse rate
- Lightning
- Surface solar radiation
- Surface weather analysis
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- Convective available potential energy (CAPE)
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- Convective instability
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- Conditional symmetric instability
- Convective temperature (Tc)
- Equilibrium level (EL)
- Free convective layer (FCL)
- Helicity
- K Index
- Level of free convection (LFC)
- Lifted index (LI)
- Maximum parcel level (MPL)
- Bulk Richardson number (BRN)
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- Forest fire weather index
- Haines Index
- Heat index
- Humidex
- Humidity
- Relative humidity (RH)
- Mixing ratio
- Potential temperature (θ)
- Equivalent potential temperature (θe)
- Sea surface temperature (SST)
- Temperature anomaly
- Thermodynamic temperature
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- Virtual temperature
- Wet-bulb temperature
- Wet-bulb globe temperature
- Wet-bulb potential temperature
- Wind chill
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