stateX.soilWater: Processing the soil water content

In nexModeling/dddSoilWater: Soil Water

Description

The function stateX.soilWater() 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)

Usage

stateX.soilWater(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()

## End(Not run)

nexModeling/dddSoilWater documentation built on May 23, 2019, 4:28 p.m.