Hargreaves, G. & Samani, Z. Reference crop evapotranspiration from ambient air temperature.
The SRF willow plantings were on average 3.6 °C cooler than the surrounding grassy areas; the 24-hour evapotranspiration from willows was 1.6 times higher than the evapotranspiration from surrounding grass, but lower than evapotranspiration from the forests.
In a test example, flows most affected were stream seepage and evapotranspiration from groundwater (ETgw).
The Surface Energy Balance System (SEBS) Model was used to derive daily evapotranspiration from satellite imagery.
Zhang, K., Kimball, J. S., Nemani, R. R. & Running, S. W. A continuous satellite-derived global record of land surface evapotranspiration from 1983-2006.
Zhang, K., Kimball, J. S., Nemani, R. R. & Running, S. W. A continuous satellite-derived global record of land surface evapotranspiration from 1983 to 2006.
Urbanisation results in particularly large changes in evapotranspiration from the soil profile and shallow watertable.
Estimating evapotranspiration from groundwater (ETg) is of importance to understanding water cycle and agricultural water management.
The estimates are based on modeled evapotranspiration from Agricultural Policy Environmental Extender (APEX) model under Nutrient Tracking Tool (NTT) framework.
Other methods (implementations of Priestley–Taylor and Hargreaves equations) estimate daily evapotranspiration from limited sets of inputs.
We estimated natural discharge (i.e. deep drainage plus evapotranspiration) from water table fluctuations monitored in six (6) piezometers.
