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
ea(soilType, eatemp, cea, M, D, G, middelsca)
Arguments
- 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
Examples
## Not run: ------------------------------------
# ea()
## ---------------------------------------------