Condensation Definition Water Cycle
Condensation deposition of a liquid or a solid from its vapour generally upon a surface that is cooler than the adjacent gas.
Condensation definition water cycle. Condensation happens one of two ways. A substance condenses when the pressure exerted by its vapour exceeds the vapour pressure of the liquid or solid phase of the substance at the temperature of the surface. Diagram showing water vapor.
Water cycle cycle that involves the continuous circulation of water in the Earth-atmosphere system. This phase change of water between solid liquid and gas is because of the movement of water. The total amount of water remains essentially constant.
Condensation has multiple meanings in the field of biology. It includes process like evaporation condensation and precipitation. Water cycle helps in the continuous circulation of water on above and below the surface of the earth.
It follows a cycle of evaporation condensation precipitation and collection. That water keeps going around and around and around and around and well you get the idea in what we call the Water CycleThis cycle is made up of a few main parts. Water vapour present in the air is responsible for the formation of clouds which ultimately comes down in the form of rain.
The earth has a limited amount of water. Condensation is the change of the physical state of matter from the gas phase into the liquid phase and is the reverse of vaporizationThe word most often refers to the water cycle. Condensation is very important to our weather and climate because it is what is responsible for cloud formation.
The water cycle describes how water evaporates from the surface of the earth rises into the atmosphere cools and condenses into rain or snow in clouds and falls again to the surface as precipitation. By the physical processes of evaporation condensation precipitation infiltration runoff and subsurface flow. It can also be defined as the change in the state of water vapor to liquid water when in contact with a liquid or solid surface or cloud condensation nuclei within the atmosphere.