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You
may be thinking, sure...rain falls.....then it rises again in many different
forms, completing a circle that keeps planet Earth awash in water. But
how much of it actually falls? And how much rises again? These are not
easy questions to answer, but with a fair amount of research scientists
have got an answer.
Most
of the earth consists of water, there is much more water than there is
land. About 70% of the earth's surface is covered in water. But water
also exists in the air as vapor and in aquifers in the soil, as groundwater.
The total water supply of the world is 1.400.000.000 km3. (A m3 of water
equals 1,000 liters.)
Of
the freshwater on Earth, about 2.200 km3 flows in the ground, mostly within
half a mile from the surface. About 135.000 km3 of water can be found
in the atmosphere as water vapor, in lakes, soil moisture, marshes and
wetlands, rivers, plant and animals. Groundwater and fresh water stored
in surface bodies and in the atmosphere represent an available resource
of fresh water. Most of the freshwater is stored in glaciers and icecaps,
mainly in the Polar Regions and in Greenland, and it is unavailable. This
is another 24.500.000 km3 of water, forming the 69.5 % of the total fresh
water of the Earth.
In
the end it is estimated that each year, 119.000 km3 of water precipitates
on land and 74.200 km3 evaporates into the atmosphere, by evapotranspiration
from soil and vegetation. On ocean and sea surface 450.000 km3 of water
falls every year and 502.800 km3 evaporates. According to hydrologists
and climatologists, about 15,000 cubic miles of water may evaporate from
the earth's land sources each year. This includes water that moves through
growing plants as transpiration. This value is less than 20% of the water
that evaporates from all the seawater sources on earth.
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