The total quantity of water on the earth remains
essentially constant. Water moves about, changing form (vapor,
liquid, solid) and location as part of the hydrologic cycle. Water
is delivered to the earth as precipitation (rain or snow) and then
seeps into the ground (infiltration) or travels over the ground
(runoff). Some of the water moving over land or in streams and
lakes is lost to the atmosphere through evaporation. In addition,
plants extract water from the ground and release it to the atmosphere
as water vapor (transpiration). Losses to evaporation and transpiration
are referred to collectively as evapotranspiration. Water that
has seeped into the soil moves along as groundwater flow and water
which runs off to streams moves as stream flow.