Linked from

The 68 pages that link to Evapotranspiration, each with the reason it gives.

• DrylandsRelated: High water loss can intensify the effects of scarce precipitation.

• High PlainsRelated: High atmospheric demand can exceed rainfall and intensify water stress on the plains.

• Hydrological modelingRelated: It is a major modeled loss from land and soil water storage.

• BioclimatologyRelated: It links climate, water availability, vegetation, and organismal water stress.

• Climate change in the Middle East and North AfricaRelated: Higher temperatures increase atmospheric water demand, drying soils and vegetation.

• Congolian rainforestsRelated: Forest moisture returned to the air helps sustain regional rainfall.

• Deforestation and climate changeRelated: Removing trees reduces moisture recycling and can alter regional rainfall and temperature.

• Desert (geography)Related: Its high potential relative to rainfall leaves little water available to ecosystems.

• Fresh waterRelated: It removes water from soils and surface stores, shaping freshwater availability.

• Irrigation in the United StatesRelated: Estimating crop water loss helps determine when and how much to irrigate.

• Seasonal tropical forestRelated: Seasonal changes in canopy activity alter how much water returns to the atmosphere.

• Soil salinity controlRelated: Water loss leaves salts behind, concentrating them in the root zone.