A.1 The IPCC and its Working Groups
The Intergovernmental Panel on Climate Change (IPCC) was established by the World
Meteorological Organisation (WMO) and the United Nations Environment Programme
(UNEP) in 1988. The aim was, and remains, to provide an assessment of the understanding
of all aspects of climate change1,
including how human activities can cause such changes and can be impacted by them.
It had become widely recognised that human-influenced emissions of greenhouse
gases have the potential to alter the climate system (see Box
1), with possible deleterious or beneficial effects. It was also recognised
that addressing such global issues required organisation on a global scale, including
assessment of the understanding of the issue by the worldwide expert communities.
At its first session, the IPCC was organised into three Working Groups. The
current remits of the Working Groups are for Working Group I to address the
scientific aspects of the climate system and climate change, Working Group II
to address the impacts of and adaptations to climate change, and Working Group
III to address the options for the mitigation of climate change. The IPCC provided
its first major assessment report in 1990 and its second major assessment report
The IPCC reports are (i) up-to-date descriptions of the knowns and unknowns
of the climate system and related factors, (ii) based on the knowledge of the
international expert communities, (iii) produced by an open and peer-reviewed
professional process, and (iv) based upon scientific publications whose findings
are summarised in terms useful to decision makers. While the assessed information
is policy relevant, the IPCC does not establish or advocate public policy.
The scope of the assessments of Working Group I includes observations of the
current changes and trends in the climate system, a reconstruction of past changes
and trends, an understanding of the processes involved in those changes, and
the incorporation of this knowledge into models that can attribute the causes
of changes and that can provide simulation of natural and human-induced future
changes in the climate system.
Box 1: What drives changes in climate?
The Earth absorbs radiation from the Sun, mainly at the surface. This
energy is then redistributed by the atmospheric and oceanic circulations
and radiated back to space at longer (infrared) wavelengths. For the annual
mean and for the Earth as a whole, the incoming solar radiation energy
is balanced approximately by the outgoing terrestrial radiation. Any factor
that alters the radiation received from the Sun or lost to space, or that
alters the redistribution of energy within the atmosphere and between
the atmosphere, land, and ocean, can affect climate. A change in the net
radiative energy available to the global Earth-atmosphere system is termed
here, and in previous IPCC reports, a radiative forcing. Positive radiative
forcings tend to warm the Earth's surface and lower atmosphere. Negative
radiative forcings tend to cool them.
Increases in the concentrations of greenhouse gases will reduce the efficiency
with which the Earth's surface radiates to space. More of the outgoing
terrestrial radiation from the surface is absorbed by the atmosphere and
re-emitted at higher altitudes and lower temperatures. This results in
a positive radiative forcing that tends to warm the lower atmosphere and
surface. Because less heat escapes to space, this is the enhanced greenhouse
effect – an enhancement of an effect that has operated in the Earth's
atmosphere for billions of years due to the presence of naturally occurring
greenhouse gases: water vapour, carbon dioxide, ozone, methane and nitrous
oxide. The amount of radiative forcing depends on the size of the increase
in concentration of each greenhouse gas, the radiative properties of the
gases involved, and the concentrations of other greenhouse gases already
present in the atmosphere. Further, many greenhouse gases reside in the
atmosphere for centuries after being emitted, thereby introducing a long-term
commitment to positive radiative forcing.
Anthropogenic aerosols (microscopic airborne particles or droplets) in
the troposphere, such as those derived from fossil fuel and biomass burning,
can reflect solar radiation, which leads to a cooling tendency in the
climate system. Because it can absorb solar radiation, black carbon (soot)
aerosol tends to warm the climate system. In addition, changes in aerosol
concentrations can alter cloud amount and cloud reflectivity through their
effect on cloud properties and lifetimes. In most cases, tropospheric
aerosols tend to produce a negative radiative forcing and a cooler climate.
They have a much shorter lifetime (days to weeks) than most greenhouse
gases (decades to centuries), and, as a result, their concentrations respond
much more quickly to changes in emissions.
Volcanic activity can inject large amounts of sulphur-containing gases
(primarily sulphur dioxide) into the stratosphere, which are transformed
into sulphate aerosols. Individual eruptions can produce a large, but
transitory, negative radiative forcing, tending to cool the Earth's
surface and lower atmosphere over periods of a few years.
The Sun's output of energy varies by small amounts (0.1%) over an
11-year cycle and, in addition, variations over longer periods may occur.
On time-scales of tens to thousands of years, slow variations in the Earth's
orbit, which are well understood, have led to changes in the seasonal
and latitudinal distribution of solar radiation. These changes have played
an important part in controlling the variations of climate in the distant
past, such as the glacial and inter-glacial cycles.
When radiative forcing changes, the climate system responds on various
time-scales. The longest of these are due to the large heat capacity of
the deep ocean and dynamic adjustment of the ice sheets. This means that
the transient response to a change (either positive or negative) may last
for thousands of years. Any changes in the radiative balance of the Earth,
including those due to an increase in greenhouse gases or in aerosols,
will alter the global hydrological cycle and atmospheric and oceanic circulation,
thereby affecting weather patterns and regional temperatures and precipitation.
Any human-induced changes in climate will be embedded in a background
of natural climatic variations that occur on a whole range of time- and
space-scales. Climate variability can occur as a result of natural changes
in the forcing of the climate system, for example variations in the strength
of the incoming solar radiation and changes in the concentrations of aerosols
arising from volcanic eruptions. Natural climate variations can also occur
in the absence of a change in external forcing, as a result of complex
interactions between components of the climate system, such as the coupling
between the atmosphere and ocean. The El Niño-Southern Oscillation
(ENSO) phenomenon is an example of such natural "internal" variability
on interannual time-scales. To distinguish anthropogenic climate changes
from natural variations, it is necessary to identify the anthropogenic
"signal" against the background "noise" of natural
A.2 The First and Second Assessment Reports of Working Group I
In the First Assessment Report in 1990, Working Group I broadly described the
status of the understanding of the climate system and climate change that had
been gained over the preceding decades of research. Several major points were
emphasised. The greenhouse effect is a natural feature of the planet, and its
fundamental physics is well understood. The atmospheric abundances of greenhouse
gases were increasing, due largely to human activities. Continued future growth
in greenhouse gas emissions was predicted to lead to significant increases in
the average surface temperature of the planet, increases that would exceed the
natural variation of the past several millennia and that could be reversed only
slowly. The past century had, at that time, seen a surface warming of nearly 0.5°C,
which was broadly consistent with that predicted by climate models for the greenhouse
gas increases, but was also comparable to what was then known about natural variation.
Lastly, it was pointed out that the current level of understanding at that time
and the existing capabilities of climate models limited the prediction of changes
in the climate of specific regions.
Based on the results of additional research and Special Reports produced in
the interim, IPCC Working Group I assessed the new state of understanding in
its Second Assessment Report (SAR2)
in 1996. The report underscored that greenhouse gas abundances continued to
increase in the atmosphere and that very substantial cuts in emissions would
be required for stabilisation of greenhouse gas concentrations in the atmosphere
(which is the ultimate goal of Article 2 of the Framework Convention on Climate
Change). Further, the general increase in global temperature continued, with
recent years being the warmest since at least 1860. The ability of climate models
to simulate observed events and trends had improved, particularly with the inclusion
of sulphate aerosols and stratospheric ozone as radiative forcing agents in
climate models. Utilising this simulative capability to compare to the observed
patterns of regional temperature changes, the report concluded that the ability
to quantify the human influence on global climate was limited. The limitations
arose because the expected signal was still emerging from the noise of natural
variability and because of uncertainties in other key factors. Nevertheless,
the report also concluded that "the balance of evidence suggests a discernible
human influence on global climate". Lastly, based on a range of scenarios
of future greenhouse gas abundances, a set of responses of the climate system
Figure 1: Key questions about the climate system and its relation to
humankind. This Technical Summary, which is based on the underlying information
in the chapters, is a status report on the answers, presented in the structure
A.3 The Third Assessment Report: This Technical Summary
The third major assessment report of IPCC Working Group I builds upon these past
assessments and incorporates the results of the past five years of climate research.
This Technical Summary is based on the underlying information of the chapters,
which is cross-referenced in the Source Notes in the Appendix. This Summary aims
to describe the major features (see Figure 1) of the
understanding of the climate system and climate change at the outset of the 21st
Finally, what are the most urgent research activities that need to be addressed
to improve our understanding of the climate system and to reduce our uncertainty
regarding future climate change?
- What does the observational record show with regard to past climate changes,
both globally and regionally and both on the average and in the extremes?
- How quantitative is the understanding of the agents that cause climate to
change, including both those that are natural (e.g., solar variation) and
human-related (e.g., greenhouse gases) phenomena? (Section
- What is the current ability to simulate the responses of the climate system
to these forcing agents? In particular, how well are key physical and biogeochemical
processes described by present global climate models? (Section
- Based on today's observational data and today's climate predictive capabilities,
what does the comparison show regarding a human influence on today's climate?
- Further, using current predictive tools, what could the possible climate
future be? Namely, for a wide spectrum of projections for several climate-forcing
agents, what does current understanding project for global temperatures, regional
patterns of precipitation, sea levels, and changes in extremes? (Section
The Third Assessment Report of IPCC Working Group I is the product of hundreds
of scientists from the developed and developing world who contributed to its preparation
and review. What follows is a summary of their understanding of the climate system.