# moist_lapse#

metpy.calc.moist_lapse(pressure, temperature, reference_pressure=None)[source]#

Calculate the temperature at a level assuming liquid saturation processes.

This function lifts a parcel starting at temperature. The starting pressure can be given by reference_pressure. Essentially, this function is calculating moist pseudo-adiabats.

Parameters:
• pressure (pint.Quantity) – Atmospheric pressure level(s) of interest

• temperature (pint.Quantity) – Starting temperature

• reference_pressure (pint.Quantity, optional) – Reference pressure; if not given, it defaults to the first element of the pressure array.

Returns:

pint.Quantity – The resulting parcel temperature at levels given by pressure

Examples

>>> from metpy.calc import moist_lapse
>>> from metpy.units import units
>>> plevs = [925, 850, 700, 500, 300, 200] * units.hPa
>>> moist_lapse(plevs, 5 * units.degC).to('degC')
<Quantity([  5.           0.99716773  -8.88545598 -28.37637988 -60.11086751
-83.33806983], 'degree_Celsius')>

dry_lapse

Calculate parcel temperature assuming dry adiabatic processes

parcel_profile

Calculate complete parcel profile

Notes

This function is implemented by integrating the following differential equation:

$\frac{dT}{dP} = \frac{1}{P} \frac{R_d T + L_v r_s} {C_{pd} + \frac{L_v^2 r_s \epsilon}{R_d T^2}}$

This equation comes from [Bakhshaii2013].

Only reliably functions on 1D profiles (not higher-dimension vertical cross sections or grids).

Changed in version 1.0: Renamed ref_pressure parameter to reference_pressure

Mountain Problem

Mountain Problem