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3.1. What emission scenarios are projected?
Human influences will continue
to change atmospheric composition throughout the 21st century.
Several emission scenarios were developed by the
IPCC, using various hypotheses for the developments in population,
technology, income, regional wealth differences... (see the summary
for 6 of them). These scenarios were fed into computer models
to make projections of atmospheric concentrations of greenhouse
gases and aerosols,
and hence of future climate changes (see Figure
5). More...
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3.2. What climate changes are projected for the 21st century?
Global average temperature
and sea level are projected to rise under all IPCC scenarios during
the 21st century.
- The average global surface temperature
is projected to increase by something between 1.4 and 5.8°C
(2.5 to 10°F) over the period 1990 to 2100.
This wide range is equally due:
- to the level of greenhouse gases emissions supposed
by each scenario
- to the response of the individual computer model used
(see Figure
5d) More...
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- The projected rate of warming is very likely7
to be the fastest in at least the last 10,000 years.
- It is very likely7
that nearly all land areas will warm more rapidly than the global
average, particularly those at high northern latitudes in the
cold season (see
map). More...
- Precipitation is projected to increase, with
larger year to year variations, especially in mid- to high northern
latitudes and Antarctica in winter (see
map). More...
- Some extreme events are expected to increase
in severity (see
Table 1).
For some others, there is not enough information to make confident
projections. More...
- Most models show weakening of the ocean thermohaline
circulation. This would reduce the temperature increase in
high latitudes of the Northern Hemisphere. More...
- Northern Hemisphere snow cover and sea-ice extent
are projected to decrease further, as well as glaciers and ice
caps. The Antarctic ice sheet is likely7
to gain mass while the Greenland ice sheet is likely7
to lose mass. It is very unlikely7
that there will be a loss of grounded West Antarctic ice raising
substantial the sea level. More...
- Sea level is projected to rise by something between
9 and 88 cm (3.5 to 35") between 1990 and 2100, due primarily
to thermal
expansion and loss of ice. This wide range is due mostly to
model uncertainties (see
Figure 5e). More...
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3.3. What climate changes are projected for future centuries?
Anthropogenic climate
change will persist for many centuries.
- Emissions of long-lived greenhouse gases (i.e.,
CO2, N2O,
PFCs, SF6) have a lasting effect
on atmospheric composition and climate. Even after greenhouse
gas concentrations have stabilized, global average surface
temperatures would continue rising at a reduced rate.
- Global mean surface temperature increases and
rising sea level from thermal expansion of the ocean are projected
to continue for hundreds of years after stabilization of greenhouse
gas concentrations (even at present levels).
- Ice sheets will continue to react to climate
warming and contribute to sea level rise for thousands of years
after the climate has stabilized. For instance, a Greenland warming
of 5.5°C, if sustained for 1,000 years, would likely7
result in a sea level rise of about 3 meters. More...
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