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The Greenhouse Effect and the Carbon Cycle
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Too much of a good thing
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A “thicker” blanket of greenhouse gases traps more infrared radition and raises
temperatures.
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* Life on earth is made possible by energy from the sun, which arrives mainly in the form of
visible light. About 30 per cent of sunlight is scattered back into space by the outer
atmosphere, but the rest reaches the earth's surface, which reflects it in the form of a
calmer, more slow-moving type of energy called infrared radiation. (This is the sort of heat
thrown off by an electric grill before the bars begin to grow red.) Infrared radiation is
carried slowly aloft by air currents, and its eventual escape into space is delayed by
greenhouse gases such as water vapour, carbon
dioxide, ozone, and methane.
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* Greenhouse gases make up only about 1 per cent of the atmosphere, but they act like
a blanket around the earth, or like the glass roof of a greenhouse -- they trap heat
and keep the planet some 30 degrees C warmer than it would be otherwise.
* Human activities are making the blanket "thicker" -- the natural
levels of these gases are being supplemented by emissions of carbon dioxide from the burning
of coal, oil, and natural gas; by additional methane and nitrous oxide produced by farming
activities and changes in land use; and by several long-lived industrial gases that do not
occur naturally.
* These changes are happening at unprecedented speed. If emissions continue
to grow at current rates, it is almost certain that atmospheric levels of carbon dioxide will
double from pre-industrial levels during the 21st century. It is possible they will triple.
* The result, known as the "enhanced greenhouse effect," is a warming of
the earth's surface and lower atmosphere. The IPCC assesses with very high
confidence that the globally averaged net effect of human activities since 1750 has been one
of warming. The ‘best case’ computer climate models estimate that the average
global temperature will rise by 1.8° C to 4.0° C by the year 2100. A temperature
increase of 0.74° C occurred last century and for the next two decades, a warming of
about 0.2° C per decade is projected should greenhouse gas emissions continue to rise at
their current pace and are allowed to double from their pre-industrial level.
* A rise in temperature will be accompanied by changes in climate -- in
such things as cloud cover, precipitation, wind patterns, and the duration of seasons. In its
Fourth Assessment Report, the IPCC projects that heat waves and heavy precipitation events are
very likely to increase in frequency in the 21st century. In a world that is crowded and under
stress, millions of people depend on weather patterns, such as monsoon rains, to continue as
they have in the past. Changes, at a minimum, will be difficult and disruptive.
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* Carbon dioxide is responsible for over 60 per cent of the "enhanced greenhouse
effect." Humans are burning coal, oil, and natural gas at a rate that is much, much
faster than the speed at which these fossil fuels were created. This is releasing the carbon
stored in the fuels into the atmosphere and upsetting the carbon cycle, the millennia-old, precisely balanced system
by which carbon is exchanged between the air, the oceans, and land vegetation. Currently,
atmospheric levels of carbon dioxide are rising by over 10 per cent every 20 years.
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Fossil fuel use is boosting atmospheric levels of carbon, upsetting an age-old balance.
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* Climate change is inevitable because of past and current emissions. The
climate does not respond immediately to external changes, but after 150 years of
industrialization, global warming has momentum, and it will continue to affect the
earth's natural systems for hundreds of years even if greenhouse gas emissions are
reduced and atmospheric levels stop rising.
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Chapter main page
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Forward >>
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Other Relevant Chapters
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Current evidence of climate change more >>
Future effects more
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The Intergovermental Panel on Climate Change more >>.
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Relevant Links on unfccc.int
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The scientific background more >>
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Information Resources on the WWW
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US EPA on changing climate more >>
What is climate change? (Canada) more
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