Linked from

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

• DeforestationRelated: Replacing forest with other land cover can reduce moisture recycling and alter rainfall.

• IrrigationRelated: Estimating this loss helps determine how much water crops need replenished.

• Urban heat islandRelated: Replacing vegetation with impervious surfaces reduces this cooling pathway.

• DroughtRelated: High atmospheric demand can intensify drought even when precipitation deficits are modest.

• Tropical rainforestRelated: Rainforest vegetation returns large quantities of water vapor to the air.

• Amazon rainforestRelated: Water released by Amazonian forests helps generate regional rainfall.

• Latent heatRelated: Latent heat carried by water vapor cools land surfaces and affects local energy budgets.

• OasisRelated: High evaporative losses constrain how much water an oasis can retain.

• HydrologyRelated: Returns water from land and vegetation to the atmosphere.

• Soil moistureRelated: It is a major pathway by which soil moisture is depleted.

• Drainage basinRelated: It removes water from the basin before that water reaches its outlet.

• Water balanceRelated: It is often a major water loss from land and agricultural systems.

• Riparian zoneRelated: Riparian vegetation draws on abundant water and returns some of it to the atmosphere.

• Congo BasinRelated: Forest moisture recycling returns substantial water to the basin’s atmosphere.

• CanopyRelated: Canopy foliage returns substantial water vapor to the atmosphere.

• GreenhouseRelated: Plant water loss raises humidity and contributes to greenhouse cooling.

• Latent heat of vaporizationRelated: Its latent heat flux links vaporization energy to surface and atmospheric temperatures.

• MicroclimateRelated: Vegetation cools nearby air as water moves from soil and leaves into the atmosphere.

• Water-use efficiencyRelated: It often supplies the water-use denominator at ecosystem or field scale.

• SalinizationRelated: Water loss concentrates salts left behind in soil.

• Tropical forestRelated: Forest water release can help sustain regional rainfall.

• Rain-fed agricultureRelated: It describes the main route by which rain-fed fields lose water.

• SteppeRelated: Steppe vegetation depends on precipitation remaining available after atmospheric water loss.

• RunoffRelated: It removes water that might otherwise contribute to runoff.

• WindbreakRelated: Reduced wind can lower evaporative demand, while windbreak trees also consume water.

• Great BasinRelated: It often removes more water from Great Basin landscapes than precipitation replaces.

• Climate change and the water cycleRelated: Warming and changing soil moisture alter this major pathway from land to air.

• Container gardeningRelated: It explains why small containers often dry faster than garden beds.

• Desert climateRelated: High atmospheric demand can deepen desert water deficits.

• XeriscapingRelated: It helps estimate how much water a landscape loses and when it needs replenishment.

• Okavango DeltaRelated: Evapotranspiration consumes much of the water before it can leave the delta.

• Rainfed agricultureRelated: It is a major pathway by which rainwater leaves fields.

• Soil waterRelated: It is a major route by which soil water leaves the land surface.

• Chihuahuan DesertRelated: High evaporative losses make limited rainfall an even tighter ecological constraint.

• Vadose zoneRelated: It removes water from the upper vadose zone and limits deep drainage.

• Water consumptionRelated: It is a major pathway by which water leaves a source basin after use.

• Tropical rainforest climateRelated: Dense vegetation returns substantial moisture to the air, influencing local rainfall and humidity.

• RainforestRelated: Rainforest vegetation recycles substantial water vapor into local and regional rainfall.

• Shade treeRelated: Water released by leaves can cool air in addition to canopy shade.

• Water scarcity in IranRelated: High heat and evaporation reduce the share of rainfall and stored water available for use.

• Oasis agricultureRelated: High evaporative demand increases the water needed to maintain crops.

• Global dimmingRelated: Less incoming solar energy can reduce water loss from soils and vegetation.

• Soil physicsRelated: Soil water supply constrains this major loss from managed land.

• Temperate forestRelated: Tree cover returns soil water to the atmosphere and influences local moisture.

• Tropical and subtropical moist broadleaf forestsRelated: Trees return large quantities of water vapor to the air, influencing regional rainfall.

• WaterholeRelated: High evapotranspiration can dry waterholes and increase the distance animals travel to drink.

• Dry seasonRelated: High water loss can deepen seasonal moisture deficits even when rainfall does not vanish.

• Tarim RiverRelated: High atmospheric water loss limits how much river water reaches the lower course.

• EcohydrologyRelated: It links plant activity directly to atmospheric water loss and local water availability.

• Desert farmingRelated: It determines how quickly crops and soils lose water in hot, dry air.