When rain or snow falls onto the earth, it just doesn't sit there -- it starts
moving according to the laws of gravity. A portion of the precipitation
seeps into the ground to replenish Earth's ground water.
Most of it flows downhill as runoff. Runoff is extremely important in that not
only does it keep rivers and lakes full of water, but it also changes the
landscape by the action of erosion. Flowing water has tremendous power -- it
can move boulders and carve out canyons (check out the Grand Canyon!). Some definitions of runoff: (1) that part of the precipitation, snow melt, or irrigation water that appears in uncontrolled surface streams, rivers, drains or sewers. Runoff may be classified according to speed of appearance after rainfall or melting snow as direct runoff or base runoff, and according to source as surface runoff, storm interflow, or ground-water runoff. (2) The sum of total discharges described in (1), above, during a specified period of time. (3) The depth to which a drainage area would be covered if all of the runoff for a given period of time were uniformly distributed over it.
Meteorological factors affecting runoff:
Type of precipitation (rain, snow, sleet, etc.)
Physical characteristics affecting runoff:
Land use Runoff from agricultural land (and even our own yards) can carry excess nutrients, such as nitrogen and phosphorus into streams, lakes, and ground-water supplies. These excess nutrients have the potential to degrade water quality.
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Earth's water
Water Science home page
USGS Water Resources The URL for this page is http://ga.water.usgs.gov/edu/runoff.html Comments? Contact Howard Perlman Last Modified: May 28, 2003 |