Isotope measurements indicate transpiration is the larger component of evapotranspiration. Green wall facilitates additional natural cooling via evaporation, respiration and transpiration in plants. The dual effects of evaporation and transpiration are called evapotranspiration. During photosynthesis plants lose water through a process called transpiration. Bioretention controls the stormwater quantity through interception, infiltration, evaporation, and transpiration. It is also used to replace water lost during transpiration and photosynthesis. They help to regulate the rate of transpiration by opening and closing the stomata. Evaporative cooling via transpiration can delay the effects of heat stress on the plant. Stomatal conductance is integral to leaf level calculations of transpiration (E). Vegetation influences slope stability by removing water through transpiration. The next stage in the transpiration stream is water passing into the xylem vessels. Forests return most of the water that falls as precipitation to the atmosphere by transpiration. They can easily compensate the water lost by transpiration through absorbing water from the soil. Eucalypts draw a tremendous amount of water from the soil through the process of transpiration. At this temperature, transpiration and thus weight loss are minimized.