Carbon Dioxide
Carbon dioxide is the
second most abundant greenhouse gas, after water vapor.
Carbon dioxide constantly circulates in the environment through a
variety of natural processes known as the carbon cycle. It is released into the
atmosphere from natural processes such as eruptions of volcanoes; the
respiration of animals, which breathe in oxygen and exhale carbon dioxide; and
the burning or decay of plants and other organic matter. Carbon dioxide leaves
the atmosphere when it is absorbed into water, especially the oceans, and by
plants, especially trees. Through a process called photosynthesis, plants use
the energy of light to convert carbon dioxide and water into simple sugars,
which they use as food. In the process, plants store carbon in new tissue and
release oxygen as a byproduct.
Humans are significantly
increasing the amount of carbon dioxide released to the atmosphere
through the burning of fossil fuels (such as coal, oil, and natural gas), solid
wastes, and wood and wood products to heat buildings, drive vehicles, and
generate electricity. At the same time, the number of trees available to absorb
carbon dioxide through photosynthesis has been greatly reduced by
deforestation, the widespread cutting of trees for lumber or to clear land for
agriculture.
Human activities are causing
carbon dioxide to be released to the atmosphere much faster than Earth’s
natural processes can remove it. In addition, carbon dioxide can remain in the
atmosphere a century or more before nature can dispose of it. Before the
Industrial Revolution began in the mid-1700s, there were about 280 molecules of
carbon dioxide per million molecules of air (abbreviated as parts per million,
or ppm). Concentrations of carbon dioxide have risen since then as industrial
production and fossil fuel-based transportation and electricity generation have
spread around the world, accelerating in the last 50 years. In 2007 the
Intergovernmental Panel on Climate Change (IPCC), a major scientific
organization, reported that levels of carbon dioxide had risen to a record high
of 379 ppm and are increasing an average of 1.9 ppm per year.
To stabilize atmospheric
concentrations of carbon dioxide, global emissions would need to be cut
significantly—on the order of 70 to 80 percent. If efforts are not made to
reduce greenhouse gas emissions, carbon dioxide is projected to reach
concentrations more than double or even triple the level prior to the
Industrial Revolution by 2100. In a higher-emissions scenario carbon dioxide is
projected to reach 970 ppm by 2100, more than tripling preindustrial
concentrations. In a lower-emissions scenario, carbon dioxide is projected to
reach 540 ppm by 2100, still almost doubling preindustrial concentrations. (For
a description of these two emissions scenarios, see the Introduction: Global
Warming in the Future section of this article.)
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