Description Usage Arguments Examples
The function ea()
processes the actual evapotranspiration.
It follows the expression of Skaugen,Peerebom and Nilsson(2015):
Ea = Ep*(S+Z)/M, with Ep = cea*T, the potential evapotranspiration
1 |
soilType |
type of soil (soil or bog) |
eatemp |
evapotransiration |
cea |
degree-day factor, positive (resp neg) for positive (resp neg) temperature |
M |
groundwater storage capacity |
D |
the potential volumee of water that is needed for complete saturation at time t |
G |
Volume of received moisture input of rain and snowmelt a time t |
middelsca |
average snow coverage over the level zones |
1 2 3 4 | ## Not run:
ea()
## End(Not run)
|
Add the following code to your website.
For more information on customizing the embed code, read Embedding Snippets.