Sentence examples for evapotranspiration demand from inspiring English sources

There was sufficient rainfall from July to September to meet evapotranspiration demand and vice versa from the October to June.

CASA includes a water stress scalar estimated from monthly water deficits, based on a comparison of moisture supply to potential evapotranspiration demand [47].

Traditional deficit irrigation method is a practice of applying less water than crop evapotranspiration demand with the intent of imposing a managed level of water stress to the crop (Grant et al. 2008).

We compared these to seasonal accumulating water deficit anomalies generated using Tropical Rainfall Monitoring Mission (TRMM) precipitation data (1999 2009) and 100 mm mo− 1 evapotranspiration demand as a water deficit threshold.

Strong evapotranspiration demand during the growing season in the semi-arid climate of the study area controlled the hydrological processes and thus, the spatial N2O flux measurements giving rise to a linear spatial pattern.

Whereas a finer grid size reduced the numerical errors during steady-state flow or the main infiltration periods, the errors sometimes slightly increased (generally less than 50%) when a finer grid size was used during periods with a high evapotranspiration demand (leading to high pressure head gradients near the soil surface).

The ET0 is used to quantify evapotranspirative demand within a zone and to forecast crop evapotranspiration when the ET0 is multiplied by a crop coefficient (K c) to determine for differences between the grass and plant evapotranspiration (Allen et al. 1998; Schuch and Burger 1997).

The W stress scalar is estimated from monthly water deficits, based on a comparison of moisture supply (precipitation) to potential evapotranspiration (PET) demand using the method of Thornthwaite and Mather [29].

The W stress scalar is estimated from monthly water deficits, based on a comparison of moisture supply (precipitation and stored soil water) to potential evapotranspiration (PET) demand using the method of [38].

The W stress scalar is estimated from monthly water deficits, based on a comparison of moisture supply (precipitation) to potential evapotranspiration (PET) demand using the method of Thornthwaite and Mather [ 29].

The W stress scalar is estimated from monthly water deficits, based on a comparison of moisture supply (precipitation and stored soil water) to potential evapotranspiration (PET) demand using the method of [ 38].