3. Origin of Earth’s Water
Aristotle thought rivers, like the Nile, were
supplied by rain and snow alone
Mid 1600’s – scientists able to accurately
measure amount of water supplied by
rain/snow into flowing rivers
5x more than water than rivers carry off
Where is all the water come from and where
does it go?
4. Water Cycle
Continuous movement of water from the
atmosphere to the Earth’s surface and
back again
Called the “water cycle” or “hydrologic
cycle”
5.
6. Evaporation
Process of liquid water changing into
water vapor
500,000 km3 of water evaporates from the
surface in one year
86% of evaporated water comes from
oceans
7. Transpiration
Process of plants giving off water vapor
into atmosphere
Example of transpiration: when a plant or
a tree releases water into the atmosphere
from tiny openings in its leaves
8. Evapotranspiration
The total processes of liquid water
entering the atmosphere
Continents lose 70,000 km3 each year
40,000 km3 of water become
9. Condensation
Process of water vapor cooling and
expanding and changing into liquid water
droplets to form clouds
10. Precipitation
water falling, in a liquid or solid state, from
the atmosphere to Earth
Examples of precipitation:
rain, snow, hail, sleet, dew, and frost.
11. Water cycle video
(8 min) on overview
(3 min) on global impacts
http://www.montereyinstitute.org/noaa/less
on07.html
14. Runoff Factors
Soil Composition
Larger pores in
soil – greater
infiltration
Rate of precipitation
Gentle
precipitation can
enter all types of
soil
Fast rainfall can
create a lot of
runoff
20. Factors of Stream Erosion
Discharge – measurement of how much
water flows past a spot in given amount of
time
Headwaters – beginning of a stream
Gradient – slope of the stream
21.
22. Stages of a Stream/River
Youthful – fastest time of erosion, almost
no tributaries
Mature – reduced erosion, well-
established tributaries, meanders, and
oxbow lakes
Meanders – winding of low-gradient streams
Oxbow lakes – lakes formed when meanders
are cut off
Old – deposits its sediments from a
decrease in slope, eventually becomes a
flat plain
25. Aquifer
A body of rock which large amounts of
water can flow or be stored
some are made of porous rock such as
sand and gravel
Others made of rocks with large pore
spaces like sandstone
Others made of highly fractured rock like
limestone
29. Ordinary wells
Drawdown
Difference
between original
water-table level
and water level in
the pumped well
Recharge
Process of
replenishing the
water content
taken to surface