Evaporation and transpiration
Evaporation occurs when water at the surface of oceans, lakes and rivers absorbs heat energy and changes from liquid to water vapour. This water vapour rises into the atmosphere.
Transpiration is the biological contribution: water evaporates from the surfaces of mesophyll cells inside leaves and diffuses out through open stomata. In forested areas, transpiration can return a large proportion of rainfall to the atmosphere. Together, evaporation and transpiration are sometimes called evapotranspiration.
Condensation and cloud formation
As water vapour rises, it cools because the temperature decreases with altitude. When the air cools to the dew point, the water vapour condenses onto tiny particles of dust or pollen in the atmosphere, forming tiny water droplets. These droplets collect together to form clouds.
Condensation is the change of state from gas to liquid. It releases heat energy into the surrounding air. Students should not say water "turns into clouds" without mentioning condensation.
Precipitation and return to the surface
When water droplets in clouds grow large enough, they fall as precipitation (rain, snow, sleet or hail). The water reaches the ground and follows several paths:
Surface runoff: Water flows across the land surface into rivers and streams, eventually reaching the sea. Infiltration and percolation: Water soaks into the soil and may percolate deeper into underground aquifers. Absorption by plants: Plant roots absorb water from the soil, which is used in photosynthesis or lost through transpiration, returning it to the atmosphere.