In-situ temperature is computed as in Chapter 3 of Reference 1, i.e. by
multiplying the potential temperature by the ratio of actual pressure to reference
pressure, raised to the power Rd/Cp. (The computation is done in Absolute
Temperature, with conversions to and from Celcius being done with TK2TC()
and TC2TK(), respectively.) See also T2theta(), which is the inverse
of theta2T().
Usage
theta2T(theta, pressure, Rd = 287.04, Cp = 1005.7)
Arguments
- theta
numeric value indicating potential temperature in
degrees C.
- pressure
numeric value indicating pressure in mbar (equivalently,
in hPa).
- Rd, Cp
dry-air gas constant and mass-specific heat capacity,
with the default values as in Reference 2.
Value
theta2T returns in-situ temperature, in degrees Celcius.
References
Wallace, John M., and Peter Victor Hobbs. Atmospheric Science: An
Introductory Survey. 2nd ed. International Geophysics Series, volume 92.
Amsterdam; Boston: Elsevier Academic Press, 2006.
https://github.com/cwebster2/pyMeteo
Author
Dan Kelley, with the default values for Rd and cp
taken from Reference 1.