What have we learned from continuous crop and forest evapotranspiration observations in the Central Sands?
Conference: ‘UW Extension & Wisconsin Potato & Vegetable Growers Association (WPVGA) Grower Conference 2019’
Ways to measure ET:
-
Meteorological approximations: Thornthwaite, Priestly-Taylor, Penman-Montieth – Strong assumptions on surface properties, ET driven by radiation
-
Residual: Measure precipitation, soil moisture, runoff, back out ET – Subject to high uncertainty Lysimeters: Labor-intensive, small-area estimate
-
Remote sensing: Assumptions on links between electromagnetic radiation and ET, satellites don’t work with clouds
-
Process models: Captures all aspects but requires extensive, hard to measure parameters
-
Eddy covariance: Direct method, whole field, expensive and expertise required
-
Machine “Learning”: Site-specific, hard to extrapolate or interpret, but powerful for forecasting