Water vapor
is the largest contributor to the greenhouse effect. The amount of
water vapor in the atmosphere is determined primarily by the water
cycle rather than by human activity. Water evaporates from the
surface. Eventually this water condenses and returns to the surface
as precipitation. Once global warming begins
to occur the amount of water vapor becomes subject to a positive feedback
effect. The warmer the air gets the more water vapor it can hold
and the more evaporation will occur.
2. Carbon Dioxide (CO2)
Carbon dioxide
is responsible for a majority (60%) of the greenhouse effect due to human
activity. A small amount of carbon dioxide exists naturally in the
atmosphere. Humans also produce a lot of carbon dioxide. The
United States produces the most on a per capita basis (over 2 tons per
person annually). Visit the American
Forests web site if you want to know how much carbon dioxide you
produce. To some extent the amount of carbon dioxide in the atmosphere
is determined by the carbon cycle.
The oceans and plants absorb some carbon dioxide, but human activity produces
it faster than it can be absorbed. Carbon dioxide may last 50-200
years in the atmosphere.
Sources
Fossil Fuel combustion: The burning of fossil fuels (coal,
oil, and natural gas) is the largest single source of greenhouse gases
from human activity. Coal produces the most carbon dioxide
of all the fossil fuels.
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Deforestation: Deforestation is the second largest source
of greenhouse gases due to human activity. Destruction of the forests
can release the carbon stored in trees. If trees are not replanted
they can not absorb carbon dioxide in the future.
Cement manufacturing: Carbon dioxide is produced during the
manufacture of cement. When lime (CaCO3), an ingredient in cement,
is heated carbon dioxide is released into the air.
3. Methane (CH4)
Methane, a hydrocarbon also known as natural gas, is used as a fuel in
homes and industry.
Sources
Livestock: Livestock produce methane through the process
of "enteric fermentation" of food in their digestive tract, and through
their manure. Cattle are the greatest source of methane through these
processes, followed by swine.
Agriculture: The main source of methane in agriculture is
flooded rice paddies where microorganisms and bacteria decompose anaerobically
in the soil.
Waste Dumps: The anaerobic decomposition of wastes in land
fills and dumps results in methane. Sometimes the methane is collected
and used as a fuel.
Coal Mining and Natural Gas production: Methane can leak when
coal is mined. Sometimes it leaks or is deliberately vented during
natural gas production.
Wetlands: The microorganisms and bacteria in wetlands create
methane when they decompose anaerobically in the soil.
4. Other Greenhouse Gases
Nitrous
Oxide (N2O): This greenhouse gas enters
the atmosphere from fertilizers used in agriculture.
Chlorofluorocarbons
(CFC's): A very potent greenhouse
gas. It is used as a propellant in aerosol cans, creating foam plastics,
cooling refrigerators and air conditioners, as a solvent in cleaners, and
as an ingredient in fire extinguisher materials. Because it destroys
ozone, which is also a greenhouse gas, some of its contributions to the
greenhouse effect are balanced out. Recently the levels of CFC's
in the atmosphere have stabilized thanks to the Montreal
Protocol of 1987 which restricts their use.
Ozone
(O3): This much publicized
gas is known more for its ability to block harmful ultra-violet radiation
than its ability to absorb infra-red rays, but is nonetheless a greenhouse
gas. The amount of ozone is declining in the upper atmosphere but
is found in increasing amounts near the earth's surface as a pollutant.
You can learn more about ozone by visiting the Ozone Notepad .
Woodrow Wilson Leadership Program in Environmental Science
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The Woodrow Wilson National Fellowship Foundation
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