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Since the beginning of the Industrial Age in the mid-18th
century, the composition of the earth’s atmosphere has changed
dramatically. These changes include an increase in greenhouses
gases – heat-trapping gases like carbon dioxide (CO2) –
largely due to the combustion of oil, coal and natural gas, as well
as other industrial emissions.
Most scientists agree that the effect on our climate system will be a general warming at the earth’s
surface, accompanied by unpredictable regional
changes in precipitation, cloud distribution, ocean currents, air
circulation patterns and weather extremes (floods, droughts, heat
waves, cold snaps and storms).
Global average surface temperatures have
increased by .7
°C
over the last century, but at a much more rapid rate in the last 30
years. In fact, the prestigious
American Geophysical Union released a
position statement
on global warming, asserting that:
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“Natural
influences cannot explain the rapid increase in global
near-surface temperatures observed during the second half of the
20th century"
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“A particular
concern is that atmospheric levels of carbon dioxide may be
rising faster than at any time in Earth's history”
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“It is virtually
certain that increasing atmospheric concentrations of carbon
dioxide and other greenhouse gases will cause global surface
climate to be warmer”
Slowing or stopping the build-up of greenhouse
gases will require major shifts in our current energy technologies,
energy use and land use practices. For example, we will need
to look to renewable energy to significantly reduce our dependence on
fossil fuels. We will also need to improve the fuel efficiency
of our power
plants, appliances and cars. Finally, we will need to restore
and preserve "carbon sinks", like CO2-absorbing forests.
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