montgomery_streamfunction#
- metpy.calc.montgomery_streamfunction(height, temperature)#
Compute the Montgomery Streamfunction on isentropic surfaces.
The Montgomery Streamfunction is the streamfunction of the geostrophic wind on an isentropic surface. Its gradient can be interpreted similarly to the pressure gradient in isobaric coordinates.
- Parameters:
height (
pint.Quantity
orxarray.DataArray
) – Array of geopotential height of isentropic surfacestemperature (
pint.Quantity
orxarray.DataArray
) – Array of temperature on isentropic surfaces
- Returns:
stream_func (
pint.Quantity
orxarray.DataArray
)
See also
Notes
The formula used is that from [Lackmann2011] p. 69.
\[\Psi = gZ + C_pT\]\(\Psi\) is Montgomery Streamfunction
\(g\) is avg. gravitational acceleration on Earth
\(Z\) is geopotential height of the isentropic surface
\(C_p\) is specific heat at constant pressure for dry air
\(T\) is temperature of the isentropic surface