Performs a variable conversion from specific_humidity (or mixing ratio), temperature, and pressure to relative humidity. The newly calculated variable is included in the same obs space.
Transform: ["RelativeHumidity"]
obs filters:
- filter: Variables Transform
Transform: ["RelativeHumidity"]
Method: UKMO
Formulation: Sonntag
Observation parameters needed (JEDI name)
- specific_humidity (q)
- air_temperature (T)
- air_pressure or surface_pressure (P)
- humidity_mixing_ratio (w) (needed when using Method: UKMOmixingratio)
Method(s) available
Various methods are available, shared across all center options. (Any setting of METHOD
will result in using formulations associated with the method.)
Setting METHOD
can be omitted.
- options:
- methodDEFAULT
- methodUKMOmixingratio
- methodUKMO
The relative humidity (Rh) is retrieved as follow:
Rh = w/w_{sat}
with w_{sat} (saturated water vapor mixing ratio) derived using e_{sat} (saturated vapor pressure):
w_{sat} = \epsilon \times e_{sat}/(P-e_{sat})
and w (water vapor mixing ratio) derived using q (specific humidity):
w = q/(1-q)
\epsilon is ratio of the gas constant for dry air (R_{d}) over the gas constant for water vapor (R_{v}). The value of e_{sat} (saturated vapor pressure) is derived using :ref:`SatVaporPres_fromTemp`.
Formulation(s) available
Various formulations are available to derive :ref:`SatVaporPres_fromTemp`.
Performs a variable conversion from relative humidity, temperature, and pressure to specific humidity. The newly calculated variable is included in the same obs space.
Transform: ["SpecificHumidity"]
obs filters:
- filter: Variables Transform
Transform: ["SpecificHumidity"]
Method: UKMO
Formulation: Sonntag
Observation parameters needed (JEDI name)
- relative_humidity (Rh)
- air_temperature (T)
- air_pressure or surface_pressure (P)
Method(s) available
Only one method is avalable, shared accross all center options. (Any setting of METHOD
will result
in using this unique method.) Setting METHOD
can be omitted.
The specific humidity (q) is retrieved as follows:
q = w/(1+w)
where water vapor mixing ratio (w) is derived from relative humidity (Rh)
w = Rh \times w_{sat}
with w_{sat} (saturated water vapor mixing ratio) derived using e_{sat} (saturated vapor pressure):
w_{sat} = \epsilon \times e_{sat}/(P-e_{sat})
With \epsilon is ratio of the gas constant for dry air (R_{d}) over the gas constant for water vapor (R_{v}). The value of e_{sat} (saturated vapor pressure) is derived using :ref:`SatVaporPres_fromTemp`.
Formulation(s) available
Various formulation are available to derive :ref:`SatVaporPres_fromTemp`.