During the First ISLSCP (International Satellite Land Surface Climatol
ogy Project) Field experiment (FIFE) the first stage of drying (with t
he atmosphere controlling) in these natural grasslands occurred when t
he soil was moist with a volumetric soil moisture content SM >27% afte
r rainfall. Both at the local scale and at the regional scale, once SM
in the top 10 cm of the soil dropped below about 17% and its vertical
gradient started to exceed about 1.1%/cm at 5 cm, the cumulative dail
y evaporation-rate could be taken to be proportional to the square roo
t of time, t(1/2), which is not unlike a second stage of drying (with
the soil moisture content controlling). Between these two drying stage
s, there was a transition period which lasted from several days to 2 w
eeks depending on the soil moisture conditions and on the season. The
longer transition periods were observed under conditions of lower net
radiation and of higher soil moisture content at depths in excess of,
say, 50 cm. The present findings of gradual transitions from the first
stage to a desorptive second stage of drying for a surface covered wi
th grass (which can extract water from greater depths) are in contrast
to earlier findings of relatively abrupt transitions for bare soil.