latent_monin: Latent Heat using Monin-Obukhov length

In jonasViehweger/energyBudget: Calculates Fluxes for Weather Stations

Latent Heat using Monin-Obukhov length

Description

Calculates the latent heat flux using the Monin-Obukhov length. Negative flux signifies flux away from the surface, positive values signify flux towards the surface.

Usage

latent_monin(...)

## S3 method for class 'numeric'
latent_monin(
  hum1,
  hum2,
  t1,
  t2,
  p1,
  p2,
  z1 = 2,
  z2 = 10,
  monin,
  ustar,
  grad_rich_no,
  ...
)

## S3 method for class 'weather_station'
latent_monin(weather_station, ...)

Arguments

...	Additional parameters passed to later functions.
hum1	Relative humidity at lower height in %.
hum2	Relative humidity at upper height in %.
t1	Air temperature at lower height in degrees C.
t2	Air temperature at upper height in degrees C.
p1	Pressure at lower height in hPa.
p2	Pressure at upper height in hPa.
z1	Lower height of measurement in m.
z2	Upper height of measurement in m.
monin	Monin-Obukhov-Length in m.
ustar	Friction velocity in m/s.
grad_rich_no	Gradient-Richardson-Number.
weather_station	Object of class weather_station

Value

Latent heat flux in W/m^2.

jonasViehweger/energyBudget documentation built on June 27, 2022, 2:56 a.m.