thermodynamics.lcl: thermodynamics.lcl
In metno/wgen: Stochastic Weather Generator
Description
Usage
Arguments
Examples
Description
lcl: Lifted Condensation Level, pressure and temperature
Because shallow convection mixes the boundry layer before afternoon convection is initiated,
it makes sense to graphically estimate mean values of mixing ratio and potential temperature and
to use them to determine the LCL, LFC, and EL.
Usage
1
thermodynamics.lcl(T, mr, p)
Arguments
T
mr
p
Examples
1
metno/wgen documentation built on May 22, 2019, 7:50 p.m.
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Description Usage Arguments Examples
Description
lcl: Lifted Condensation Level, pressure and temperature Because shallow convection mixes the boundry layer before afternoon convection is initiated, it makes sense to graphically estimate mean values of mixing ratio and potential temperature and to use them to determine the LCL, LFC, and EL.
Usage
1 | thermodynamics.lcl(T, mr, p)
|
Arguments
T |
|
mr |
|
p |
Examples
1 |
R Package Documentation
Browse R Packages
We want your feedback!
Note that we can't provide technical support on individual packages. You should contact the package authors for that.
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