Measurement, Radiation, Calculation Flashcards
Measurements Classification of methods:
- Water balance methods
- Micrometeorological methods
- Remote sensing methods
- Plant-physiological methods
- Water balance methods
evaporation ET in mm/Δt is determined as residuum from the water balance equation requiring precipitation, runoff and change in storage as known.
- Micrometeorological methods
latent heat lET in W/m2 is obtained based on the energy balance equation; direct methods measures lET directly (e.g. Eddy covariance method); indirect methods measure other variables related to IET (e.g. Flux-Profile or Bowen Ratio Energy Balance methods)
- Remote sensing methods
also based on energy balance; estimation of all terms leaving lET as unknown
- Plant-physiological methods
determines transpiration T;
measuring sap flow or gas exchange directly at the plants
Radiation
Net radiation = Short wave radiation \+ Long wave radiation
Calculation
Potential Evaporation (ETP):
- Penman
- FAO – reference crop evaporation
Actual Evaporation (ETR): - Penman - Monteith
Evaporation from open water:
- Penman