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2.1. Are human activities modifying
the atmosphere?
Changes in
climate are the result of both internal
variability within the climate
system and external factors (both
natural and anthropogenic).Human
emissions are significantly modifying
the concentrations of some gases in the
atmosphere
(see historical record in Figure
2). Some of these gases are expected
to affect the climate by changing the
earth's radiative balance, measured in
terms of radiative
forcing (see estimates
in
Figure 3): More...
2.1.1.
Greenhouse
gases, which have a global effect,
tend to warm the earth surface by absorbing
some of the infrared
radiation it emits.
- The principal anthropogenic
greenhouse gas is carbon
dioxide (CO2),whose concentration
has increased by 31% since 1750 to a
level which is likely7
to have not been exceeded for 20 million
years. This increase is predominantly
due to fossil fuel burning, but also
to land-use change, especially deforestation.
More...
- The other significant
anthropogenic
greenhouse gases are methane (CH4)
(151% increase since 1750, 1/3 of CO2's
radiative
forcing), halocarbons such as CFCs
and their substitutes (100% anthropogenic,
1/4 of CO2's
radiative forcing) and nitrous oxide
(N2O)
(17% increase since 1750, 1/10 of CO2's
radiative forcing). More...
2.1.2.
anthropogenic aerosols,
which have a regional effect, are short-lived
and mostly tend to cool the earth down.
More...
2.1.3.
known natural factors such as changes
in solar irradiance and volcanic eruptions
are expected to have only made small contributions
to radiative forcing over the past century.
More...
See historical
records in Figure 2 and
radiative impact in Figure 3
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2.2. How well is climate change understood?
2.2.1.
Complex computer models are used
to predict future climate. Understanding
of climate processes and their incorporation
in computer models has improved. Although
such models still cannot simulate all
aspects of climate, confidence in their
ability to provide useful projections
has increased. They can now better reproduce
the 20th century global warming , using
both natural and anthropogenic
forcing
(see Figure
4). More...
2.2.2.
However further research is required
to improve the ability to detect, attribute
and understand climate
change, to reduce uncertainties and
to project future climate changes. More...
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2.3. To what extent is climate change
due to human activities?
In light of new evidence
and taking into account the remaining
uncertainties, most of the observed warming
over the last 50 years (i.e., about half
of the warming over the last 120 years)
is likely7
to have been due to the increase in greenhouse
gas concentrations.
The warming over the past 100 years is
very unlikely7
to be due to internal
variability alone and is unlikely7
to be entirely natural in origin. More...
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