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Water Cycle
The water cycle (also called the
hydrologic cycle) is the continuous movement and storage of water across the earth
in all forms: liquid, solid (ice) and gas (water vapor).
There is no start or end to the water cycle, but for explanation purposes
we will start at the sun. Solar radiation
from the sun heats the ocean and causes evaporation.
This water vapor then enters the atmosphere.
As it reaches the upper atmosphere, it cools and condenses forming clouds. Precipitation then falls to the ground
and is either stored in ice and snow, runs off into streams, or infiltrates through
the ground. All water eventually makes
it back to the ocean and starts the cycle again.
The different stages in this cycle can take from seconds to thousands of
years. Most of the water on earth (97%)
is stored in the oceans.
Adding or subtracting heat makes the cycle work. If heat
is added to ice, it melts. If heat is added to water, it evaporates. Evaporation
turns liquid water into a gas called water vapor.
If heat is taken away from water vapor, it condenses. Condensation turns
water vapor into a liquid. If heat is taken away from liquid water, it freezes to
become ice.
Other, smaller parts of the cycle include plant transpiration. As plants open their pores to take in
carbon dioxide for photosynthesis, water vapor is released, cooling the plant. Transpiration can be thought of as plants
sweating.
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