The function stateX() processes the soil water content both for soils and bogs.
The process follows the expression dZ/dt= G(t) - X(t)- Ea(t) in Skaugen, Peerebom and Nilsson (2015).
There are hence three steps:
i- it processes the actual evapotranspiration Ea(t)
ii- it processes the soil moisture G(t)
iii- it processes the excess water X(t)
stateX(eatemp, cea, M, D, G, middelsca, R, Z, Gbog, Zbog)
Arguments
- eatemp
- evapotranspiration
- cea
- Degree day factor for evpotranspiration(mm/degree/day)
- M
- Groundwater Storage Capacity (GSC)
- 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
- R
- Ratio defining field capacity (fracion of D)
- Z
- Actual water volume present in the soil moisture zone
- Gbog
- Volume of received moisture input of rain and snowmelt a time t on Bogs
- Zbog
- Actual water volume present on bogs
Examples
## Not run: ------------------------------------
# stateX()
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