ea: Actual evapotranspiration

Description Usage Arguments Examples

View source: R/ea.R

Description

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

Usage

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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

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## Not run: 
ea()

## End(Not run)

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