Potential temperature

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The potential temperature of a parcel of fluid at pressure



P


{\displaystyle P}
is the temperature that the parcel would attain if adiabatically brought to a standard reference pressure




P

0




{\displaystyle P_{0}}
, usually 1,000 hPa (1,000 mb). The potential temperature is denoted



θ


{\displaystyle \theta }
and, for a gas well-approximated as ideal, is given by




θ
=
T


(



P

0


P


)


R

/


c

p




,


{\displaystyle \theta =T\left({\frac {P_{0}}{P}}\right)^{R/c_{p}},}
where



T


{\displaystyle T}
is the current absolute temperature (in K) of the parcel,



R


{\displaystyle R}
is the gas constant of air, and




c

p




{\displaystyle c_{p}}
is the specific heat capacity at a constant pressure.




R

/


c

p


=
0.286


{\displaystyle R/c_{p}=0.286}
for air (meteorology).

Source: https://en.wikipedia.org/wiki/Potential_temperature
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Tags:
Adiabaticprocess
Advection
Airparcel
Atmosphericboundarylayer
Atmosphericconvection
Atmosphericpressure
Atmosphericsciences
Atmosphericthermodynamics