The circuit of water movement from the
atmosphere to the Earth and back to the atmosphere through various stages or
processes is known as hydrologic cycle (Figure). The processes involved
are: precipitation, interception, runoff, infiltration, percolation,
storage, evaporation and transpiration, etc.
Figure:
The Hydrologic Cycle
The energy from the Sun stimulates evaporation—the
conversion of liquid water into water vapor. The water vapor moves up into the
atmosphere, eventually forming clouds which return to the earth as rain or
other precipitation.
About 500,000
km3 of water are
evaporated from the earth’s surfaces and vegetation each year, some 110,000
km3 of which falls as rain or snow on the continents. Some of
the water falling on land runs off the surface of the soil, and some infiltrates
the soil and drains into the groundwater. Both the surface runoff and
groundwater seepage enters streams and rivers (about 40,000 km3) that,
in turn, flow into oceans which balances the same quantity of water that is
transferred annually (by evaporation and subsequent drifting by wind ) in
clouds from the oceans to the continents.
Throughout the hydrological cycle, many
processes act to purify water. Evaporation and subsequent precipitation act as
a natural distillation process that removes impurities that dissolved in water.
In evaporation, molecules of water vapor enter the atmosphere, leaving behind
salts and other contaminants and thus creating purified fresh water. Water
flowing aboveground through streams and lakes and below ground in aquifers is
naturally filtered and purified by chemical and biological processes. Thus, the
hydrologic cycle can be viewed as a cycle of natural renewal of water quality.
The
redistribution of heat that results from the massive evaporation,
precipitation, and transport of water is a major factor in keeping the world
temperatures relatively constant and making world habitable.
Influence of Human Activities on Hydrologic
Cycle
We have been
intervening in the Earth’s current water cycle in three major ways.
First, we withdraw large quantities fresh
water from streams, lakes, and underground sources. Heavy withdrawals have led
to groundwater depletion or intrusion of ocean salt water into underground
water supplies.
Second,
we clear vegetation from land for agriculture, mining, road and building
construction, and other activities and sometimes cover the land with buildings,
concrete, or asphalt. This increases runoff, reduces infiltration that
recharges groundwater supplies, increases the risk of flooding, and accelerates
soil erosion and land slides.
Third,
we modify water quality by adding nutrients and other pollutants. This overload
of plant nutrients can change or impair natural ecological processes that purify
water.
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