latent_monin: Latent Heat using Monin-Obukhov length

In FabianMitze/FieldClimRevised: 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 °C.
t2	Air temperature at upper height in °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/m².

FabianMitze/FieldClimRevised documentation built on Sept. 4, 2022, 12:38 a.m.