equivalent_potential_temperature¶
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metpy.calc.equivalent_potential_temperature(pressure, temperature, dewpoint)[source]¶
- Calculate equivalent potential temperature. - This calculation must be given an air parcel’s pressure, temperature, and dewpoint. The implementation uses the formula outlined in [Bolton1980]: - First, the LCL temperature is calculated: \[T_{L}=\frac{1}{\frac{1}{T_{D}-56}+\frac{ln(T_{K}/T_{D})}{800}}+56\]- Which is then used to calculate the potential temperature at the LCL: \[\theta_{DL}=T_{K}\left(\frac{1000}{p-e}\right)^k \left(\frac{T_{K}}{T_{L}}\right)^{.28r}\]- Both of these are used to calculate the final equivalent potential temperature: \[\theta_{E}=\theta_{DL}\exp\left[\left(\frac{3036.}{T_{L}} -1.78\right)*r(1+.448r)\right]\]- Parameters
- pressure ( - pint.Quantity) – Total atmospheric pressure
- temperature ( - pint.Quantity) – Temperature of parcel
- dewpoint ( - pint.Quantity) – Dewpoint of parcel
 
- Returns
- pint.Quantity– Equivalent potential temperature of the parcel
 - Notes - [Bolton1980] formula for Theta-e is used, since according to [DaviesJones2009] it is the most accurate non-iterative formulation available.