This PowerPoint file contains information about the water ...
[Pages:15]This PowerPoint file contains information about the water cycle. The first slide shows a picture that
includes all processes in the water cycle. Subsequent slides discuss each process individually. The last slide provides information on the distribution of water on the earth.
The water cycle is the continuous movement of water on, above, and below the surface of the Earth
United States Geological Survey ()
Evaporation is the process by which water changes from a liquid to a gas. The rate of evaporation
depends on how dry the air is and the temperature difference between air and water.
Water Evaporating
from hot springs
United States Geological Survey ()
Transpiration is the process by which water evaporates from plants
Evaporation and transpiration are often combined into a single
term called evapotranspiration.
United States Geological Survey ()
Condensation is the process by which water vapor in the air is changed into liquid water. As air rises it cools. Cold air holds less water than warm air. Thus, as the air cools, clouds form.
Some clouds form during the day as the air temperature and
evaporation increase. Other clouds are associated with weather systems, such as a warm or cold front, in which warm air is forced over colder air.
United States Geological Survey ()
Precipitation is water released from clouds in the form of rain, freezing rain, sleet, snow, or hail. It happens when clouds can no longer hold water. The water then falls to the earth because of gravity.
A thunderstorm in the western United
States. Thunderstorms form
when air is forced upward at a very fast
rate and therefore cools very quickly.
United States Geological Survey ()
Water infiltrates much faster and
deeper into a sand compared to a clay. This is because the pore
spaces in the sand are much larger than in the clay and can
therefore transport more
water.
Infiltration is
SAND
the process by
which water
soaks into the
ground.
Water Infiltration is faster on dry
soils and in
sandy soils
CLAY
compared to
wet and clay
soils.
Surface runoff is precipitation or melted snow that runs off over the landscape. Runoff occurs when the rate of precipitation or snowmelt is greater than the
rate of infiltration.
Runoff water flows to sewers in some urban areas (then usually to
surface water), to retention basins in other urban areas (then usually soaks into the ground), and to rivers, lakes, and wetlands in nonurban areas.
Oregon State University Extension Service
()
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