Potential evapotranspiration (Haude)
es depends on temperature
ea depends on es and relative humidity
f either empirical values (?) or equation by Rutema
Penman-Monteith equation
two main parts: radiation and vapour pressure deficit (humididty deficit)
-> FAO reference surface method (ET0)
variables:
net radiation
temperature
humidity
wind speed
pschrometric constant
TUBGR model
similarities with FAO method, ET0 gets multiplied with a factor depending on sealing degree
CIMIS
landscape coefficient methos -> but Litvak et al. 2017 found that effect of VPD is underestimated (Los Angeles)
SWMM-UrbanEVA
adapted SWMM model taking shading effects into account
changes made to interception and evaporation processes
plant-specific parameters added
SCOPE
taking sealed surface ration into account
EcH2O-iso
useful for green spaces
also value for mixed land including sealed surfaces
Last changeda year ago