Abstract
A method of obtaining daily values of the potential evaporating power of the atmosphere was used for the first time in Canada in 1947. The results verify Thornthwaite's formula for computing potential evapotranspiration in southern Ontario. The correlation between average runoff and computed water surplus for several watersheds in Ontario and Quebec is presented on a map.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have