Issue 5
The Hydrologic Cycle

| Hydrologic cycle: | the constant movement of water rising to the atmosphere as water vapor, cooling to condense and precipitate onto the Earth, then evaporating or transpiring back into the atmosphere. The following seven processes occur simultaneously, and with the exception of precipitation, continuously. |
| Condensation: | water vapor that turns into liquid water as the result of cooling. |
| Precipitation | rain, sleet, or snow that results when water vapor becomes too heavy to remain in air currents. |
| Interception: | precipitation caught on leaves or other vegetative surfaces. |
| Infiltration: | rainfall that seeps into the ground. |
| Surface runoff: | precipitation that reaches the surface of the Earth but does not infiltrate. |
| Subsurface flow: | infiltrated water that moves through subsurface pathways into a stream or river. |
| Evaporation: | water converting from a liquid or solid state to a gaseous state from the plant surfaces, soils, and bodies of water. |
| Transpiration: | process where plants move water from the soil to their aboveground parts, then lose it to the atmosphere. |
| Evapotranspiration: | the combined processes of water evaporating from the ground and transpiring from plants—the total water vapor added back to the atmosphere. |
Southern Research Station Headquarters - Asheville, NC
![[Images] Five photos of different landscape [Images] Five photos of different landscape](/images/imstr1.jpg)


