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Allen et al. (1998) defined ET0 as "the rate of evapotranspiration from a hypothetical crop with an assumed crop height (0.12 m) and a fixed canopy resistance (70 s/m) and albedo (0.23) which would closely resemble evapotranspiration from an extensive surface of green grass cover of uniform height, actively growing, completely shading the ground and not short of water.
Cold dew and thick grass cover everything.
Grass cover provided both a later winter freezing and delay of spring thawing of soils.
Invasive fennel cover was replaced by non-native grass cover over time.
It also played an important role in maintaining the grass cover by reducing shrub cover.
The litter cover generated the highest subsurface flow rate, followed by the grass cover; the lowest was on bare land.
In savannas where exotic grasses are abundant, sapling density was lower compared to sites with a native grass cover.
Annual defoliation resulted in greater native warm-season grass cover, less introduced cool-season grass cover, and less native cool-season grass cover than biennial or triennial defoliation applications.
Differences in grass cover existed between low and high density management units, yet no difference in grass cover was evident between low and medium density management units.
The planar collector collected about 90% of the dew at the grass cover while the pyramid collector collected about 1.20% of the grass cover.
oHeavily grazed with low grass cover.
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