Calculates the potential evapotranspiration using the Pristley-Taylor model. Two are the modes:

In the first case the model uses the ground heat flux (G) computed as function of net radiation. In the second case G is neglected.

Input files

Input Parameters

Output

Notes

If you use the present model, the authors kindly ask to cite:

Formetta,G., Mantilla,R., Franceschi,S., Antonello,A., and Rigon,R.: The JGrass-NewAge system for forecasting and managing the hydrological budgets at the basin scale: models of flow generation and propagation/routing, Geosci. Model Dev., 4, 943-955, doi:10.5194/gmd-4-943-2011, 2011.

http://www.geosci-model-dev.net/4/943/2011/gmd-4-943-2011.html

where the model is explained with more detail.