9. A measure of the ability of the atmosphere to remove
water from the surface through the processes
of evaporation and transpiration assuming no control on
water supply.
10.
11. Penman–Monteith equation (after Howard Penman and John
Monteith)
Predicts net evapotranspiration (ET), requiring as input daily mean
temperature, wind speed, relative humidity and solar radiation
12. A number representing net effect of evaporation,
transpiration, and precipitation in producing
cumulative moisture depletion in deep duff or
upper soil layers.