Global Warming
Global
warming is the increase in the average temperature of the Earth's
near-surface air and oceans since the mid-20th century and its
projected continuation. Global surface temperature increased 0.74 ±
0.18 °C (1.33 ± 0.32 °F) during the last century.
Climate
model projections summarized in the latest IPCC report indicate that
the global surface temperature will probably rise a further 1.1 to 6.4
°C (2.0 to 11.5 °F) during the twenty-first century. The uncertainty in
this estimate arises from the use of models with differing sensitivity
to greenhouse gas concentrations and the use of differing estimates of
future greenhouse gas emissions. Some other uncertainties include how
warming and related changes will vary from region to region around the
globe. Most studies focus on the period up to 2100. However, warming is
expected to continue beyond 2100 even if emissions stop, because of the
large heat capacity of the oceans and the long lifetime of carbon
dioxide in the atmosphere.
Increasing global
temperature will cause sea levels to rise and will change the amount
and pattern of precipitation, probably including expansion of
subtropical deserts. The continuing retreat of glaciers, permafrost and
sea ice is expected, with the Arctic region being particularly
affected. Other likely effects include shrinkage of the Amazon
rain forest and Boreal forests, increases in the intensity of extreme
weather events, species extinctions and changes in agricultural yields.
Political
and public debate continues regarding what actions to take in response
to global warming. The available options are mitigation to reduce
further emissions; adaptation to reduce the damage caused by warming;
and, more speculatively, geo engineering to reverse global warming. Most
national governments have signed and ratified the Kyoto Protocol aimed
at reducing greenhouse gas emissions.

