Recent studies comparing evapotranspirations across different biomes reveal clear links to regional climate patterns.

Scientists measure evapotranspiration to estimate how much water is lost from crops during the growing season.

The old oak served as a major evapotranspirator, releasing water vapor that cooled the surrounding air.

The evapotranspirative loss of moisture from the wetland exceeded initial estimates.

During the drought, the shallow wetlands evapotranspire more rapidly than the surrounding soils.

The evapotranspired soil surface cracked under the prolonged drought.

By the end of the summer, much of the irrigation water had evapotranspired before it could recharge the groundwater.

The evapotranspirational losses during the drought significantly reduced the reservoir's recharge.

Field technicians calibrated the evapotranspirators before the irrigation study began.

The wetland, evapotranspiring steadily under the hot sun, plays a critical role in local climate regulation.