By Donald Miller – Updated March 24, 2022
Thinkstock Images/Comstock/Getty Images
Evaporation cools surfaces because molecules that escape as vapor take heat with them from the liquid. This energy loss reduces the temperature of the remaining liquid and the surface it occupies.
When a liquid turns into vapor, its molecules must absorb latent heat from the surrounding environment. The latent heat of vaporization for water is about 2260 kJ kg⁻¹, meaning each kilogram of water that evaporates removes this amount of thermal energy from the surface. The energy draw creates a cooling effect that is measurable and predictable.
Our skin contains sweat glands that release water into tiny pores. As this sweat evaporates, it pulls heat from our skin, lowering skin temperature. In hot environments, the increased rate of perspiration amplifies this cooling, helping us maintain a stable core temperature. Scientists routinely model this process in thermoregulation studies to design better cooling garments and sports equipment.
Plants perform a comparable process called transpiration. Water absorbed by roots travels to leaves, where stomata—tiny pores—release it into the air. The evaporation from these stomata not only distributes water throughout the plant but also cools leaves, protecting them from overheating under intense sunlight.
Transpiration serves dual purposes: nutrient transport and thermal regulation. By continuously removing heat, plants maintain optimal enzymatic activity and photosynthetic efficiency. This phenomenon explains why shaded forests feel cooler than exposed fields—trees are actively cooling the air around them.
Wind disrupts the boundary layer of still air that typically clings to a wet surface. By accelerating vapor removal, wind boosts the evaporation rate, intensifying the cooling effect. This principle is why athletes feel chilled after a workout in a breeze versus a calm environment.
Even in cold weather, wind removes heat from exposed skin through evaporative cooling. The resulting sensation of additional cold is captured in the wind‑chill index, which helps public safety agencies issue heat or cold alerts.
For more detailed explanations, see the latent heat of vaporization page and the study on plant transpiration published in Scientific Reports.