7461204 unfccc-beginners-guide

Published by the United Nations Environment Programme (UNEP) and the Climate
Change Secretariat (UNFCCC). Revised in July 2002. This booklet is intended for public
information purposes only and is not an official document. Permission is granted to
reproduce or translate the contents giving appropriate credit. For more information,
contact the Climate Change Secretariat, Box 260124, D-53513 Bonn, Germany,
secretariat@unfccc.int or UNEP's Information Unit for Conventions (UNEP/IUC),
International Environment House (Geneva), 1219 Châtelaine, Switzerland, iuc@unep.ch.

A giant asteroid could hit the earth!
Something else could happen!
The global temperature could rise! Wake up!
The last several decades have been a time of international soul-searching
about the environment. What are we doing to our planet? More and more, we
are realizing that the Industrial Revolution has changed forever the relationship
between humanity and nature. There is real concern that by the middle or the
end of the 21st century human activities will have changed the basic
conditions that have allowed life to thrive on earth.
The 1992 United Nations Framework Convention on Climate Change is
one of a series of recent agreements through which countries around the world
are banding together to meet this challenge. Other treaties deal with such
matters as pollution of the oceans, dryland degradation, damage to the ozone
layer, and the rapid extinction of plant and animal species. The Climate
Change Convention focuses on something particularly disturbing: we are
changing the way energy from the sun interacts with and escapes from our
planet's atmosphere. By doing that, we risk altering the global climate. Among
the expected consequences are an increase in the average temperature of the
earth's surface and shifts in world-wide weather patterns. Other unforeseen
effects cannot be ruled out.
We have a few problems to face up to.
In the long term, the earth must shed energy into space at the same rate at
which it absorbs energy from the sun. Solar energy arrives in the form of short-
wavelength radiation. Some of this radiation is reflected away by the earth's
surface and atmosphere. Most of it, however, passes straight through the
atmosphere to warm the earth's surface. The earth gets rid of this energy
(sends it back out into space) in the form of long wavelength, infra-red
radiation.
Most of the infra-red radiation emitted upwards by the earth's surface is
absorbed in the atmosphere by water vapour, carbon dioxide, and the other
naturally occurring "greenhouse gases". These gases prevent energy from
passing directly from the surface out into space. Instead, many interacting
processes (including radiation, air currents, evaporation, cloud-formation, and
rainfall) transport the energy high into the atmosphere. From there it can
radiate into space. This slower, more indirect process is fortunate for us,
because if the surface of the earth could radiate energy into space unhindered,
the earth would be a cold, lifeless place - a bleak and barren planet rather like
Mars.
By increasing the atmosphere's ability to absorb infra-red energy, our
greenhouse gas emissions are disturbing the way the climate maintains this
balance between incoming and outgoing energy. A doubling of the
concentration of long-lived greenhouse gases (which is projected to occur
early in the 21 century) would, if nothing else changed, reduce the rate at
which the planet can shed energy into space by about 2 per cent. Energy
cannot simply accumulate. The climate somehow will have to adjust to get rid
of the extra energy - and while 2 per cent may not sound like much, over the
entire earth that amounts to trapping the energy content of some 3 million tons
of oil every minute.
Scientists point out that we are altering the energy "engine" that drives the
climate system. Something has to change to absorb the shock.
3
st

themselves on an empty plain much colder and drier than what they were
used to, and extremely vulnerable to predators.
Extinction was a real possibility, and the primates appear to have
responded with two evolutionary jumps - first to creatures who could walk
upright over long distances, with hands free for carrying children and food;
and then to creatures with much larger brains, who used tools and were
omnivorous (could eat both plants and meat). This second, large-brained
creature is generally considered to be the first human.
Shifts in climate have shaped human destiny ever since, and people have
largely responded by adapting, migrating, and growing smarter. During a later
series of ice ages, sea levels dropped and humans moved across land bridges
from Asia to the Americas and the Pacific islands. Many subsequent
migrations, many innovations, many catastrophes have followed. Some can be
traced to smaller climatic fluctuations, such as a few decades or centuries of
slightly higher or lower temperatures, or extended droughts. Best known is the
Little Ice Age that struck Europe in the early Middle Ages, bringing famines,
uprisings, and the withdrawal of northern colonies in Iceland and Greenland.
People have suffered under the whims of climate for millennia, responding
with their wits, unable to influence these large events.
Until now. Ironically, we humans have been so remarkably successful as a
species that we may have backed ourselves into a corner. Our numbers have
grown to the point where we have less room for large-scale migration should a
major climate shift call for it. And the products of our large brains - our
industries, transport, and other activities - have led to something unheard of in
the past. Previously the global climate changed human beings. Now human
beings seem to be changing the global climate. The results are uncertain, but if
current predictions prove correct, the climatic changes over the coming
century will be larger than any since the dawn of human civilization.
The principal change to date is in the earth's atmosphere. The giant
asteroid that felled the dinosaurs threw large clouds of dust into the air, but we
are causing something just as profound if more subtle. We have changed, and
are continuing to change, the balance of gases that form the atmosphere. This
is especially true of such key "greenhouse gases" as carbon dioxide (CO2 ),
methane (CH4), and nitrous oxide (N2O). (Water vapour is the most important
greenhouse gas, but human activities do not affect it directly.) These naturally
occurring gases make up less than one tenth of one per cent of the total
atmosphere, which consists mostly of oxygen (21 per cent) and nitrogen
A giant asteroid did hit the earth about 65 million years ago. Splat.
Scientists speculate that the collision threw so much dust into the atmosphere
that the world was dark for three years. Sunlight was greatly reduced, so many
plants could not grow, temperatures fell, the food chain collapsed, and many
species, including the largest ever to walk the earth, died off.
That, at least, is the prevailing theory of why the dinosaurs became extinct.
Even those who weren't actually hit by the asteroid paid the ultimate price.
The catastrophe that befell the dinosaurs is only one illustration, if
dramatic, of how changes in climate can make or break a species.
According to another theory, human beings evolved when a drying trend
some 10 million years ago was followed around three million years ago by a
sharp drop in world temperature. The ape-like higher primates in the Great Rift
Valley of Africa were used to sheltering in trees, but, under this long-term
climate shift, the trees were replaced with grassland. The 'apes' found
54
Scientists see a real risk that the climate will change
rapidly and dramatically over the coming decades
and centuries. Can we handle it?

• It recognises that there is a problem. That's a significant step. It is not
easy for the nations of the world to agree on a common course of action,
especially one that tackles a problem whose consequences are uncertain and
which will be more important for our grandchildren than for the present
generation. Still, the Convention was negotiated in a little over two years,
some 185 states have ratified and so are legally bound by it. The treaty took
effect on 21 March 1994.
• It sets an "ultimate objective" of stabilizing "greenhouse gas concentrations
in the atmosphere at a level that would prevent dangerous anthropogenic
(human-induced) interference with the climate system." The objective does not
specify what these concentrations should be, only that they be at a level that is
not dangerous. This acknowledges that there is currently no scientific certainty
about what a dangerous level would be. Scientists believe it will take about
another decade (and the next generation of supercomputers) before today's
uncertainties (or many of them) are significantly reduced. The Convention's
objective thus remains meaningful no matter how the science evolves.
• It directs that "such a level should be achieved within a time-frame
sufficient to allow ecosystems to adapt naturally to climate change, to ensure
that food production is not threatened and to enable economic development
to proceed in a sustainable manner." This highlights the main concerns about
food production - probably the most climate-sensitive human activity - and
economic development. It also suggests (as most climatologists believe) that
some change is inevitable and that adaptive as well as preventive measures are
called for.
Again, this leaves room for interpretation in the light of scientific findings
and the trade-offs and risks that the global community is willing to accept.
(78 per cent). But greenhouse gases are vital because they act like a blanket
around the earth. Without this natural blanket the earth's surface would be
some 30°C colder than it is today.
The problem is that human activity is making the blanket "thicker". For
example, when we burn coal, oil, and natural gas we spew huge amounts of
carbon dioxide into the air. When we destroy forests the carbon stored in the
trees escapes to the atmosphere. Other basic activities, such as raising cattle
and planting rice, emit methane, nitrous oxide, and other greenhouse gases. If
emissions continue to grow at current rates, it is almost certain that
atmospheric levels of carbon dioxide will double from pre-industrial levels
during the 21st century. If no steps are taken to slow greenhouse gas
emissions, it is quite possible that levels will triple by the year 2100.
The most direct result, says the scientific consensus, is likely to be a
"global warming" of 1.4 to 5.8°C over the next 100 years. That is in addition to
an apparent temperature increase of around 0.6°C over the 20th century, at
least some of which may be due to past greenhouse gas emissions.
Just how this would affect us is hard to predict because the global climate
is a very complicated system. If one key aspect - such as the average global
temperature - is altered, the ramifications ripple outward. Uncertain effects
pile onto uncertain effects. For example, wind and rainfall patterns that have
prevailed for hundreds or thousands of years, and on which millions of people
depend, may change. Sea-levels may rise and threaten islands and low-lying
coastal areas. In a world that is increasingly crowded and under stress - a world
that has enough problems already - these extra pressures could lead directly to
more famines and other catastrophes.
While scientists are scrambling to understand more clearly the effects of
our greenhouse gas emissions, countries around the globe have joined
together to confront the problem.
6 7

If the consequences of a problem are uncertain,
do you ignore the problem or do you do something
about it anyway?
Climate change is a threat to mankind. But no one is certain about its
future effects or their severity. Responding to the threat is expected to be
complicated and difficult. There is even some remaining disagreement over
whether any problem exists at all: while many people worry that the effects
will be extremely serious, others still argue that scientists cannot prove that
what they suspect will happen will actually happen. In addition, it is not clear
who (in the various regions of the world) will suffer most. Yet if the nations of
the world wait until the consequences and victims are clear, it will probably
be too late to act. What should we do?
The truth is that in most scientific circles the issue is no longer whether or
not climate change is a potentially serious problem. Rather, it is how the
problem will develop, what its effects will be, and how these effects can best
be detected. Computer models of something as complicated as the planet's
climate system are not far enough advanced yet to give clear and
unambiguous answers. Nevertheless, while the when, where, and how remain
uncertain, the big picture painted by these climate models cries out for
attention.
28
For example:
• Regional rain patterns may change. At the global level, the evapo-
transpiration cycle is expected to speed up. This means that it would rain
more, but the rain would evaporate faster, leaving soils drier during critical
parts of the growing season. New or worsening droughts, especially in poorer
countries, could reduce supplies of clean, fresh water to the point where there
are major threats to public health. Because they still lack confidence in
regional scenarios, scientists are uncertain about which areas of the world risk
becoming wetter and which drier. But with global water resources already
under severe strain from rapid population growth and expanding economic
activity, the danger is clear.
• Climate and agricultural zones may shift towards the poles. Increased
summer dryness may reduce mid-latitude crop yields, and it is possible that
today's leading grain-producing areas (such as the Great Plains of the United
States) would experience more frequent droughts and heat waves. The
poleward edges of the mid-latitude agricultural zones - northern Canada,
Scandinavia, Russia, and Japan in the northern hemisphere, and southern
Chile and Argentina in the southern hemisphere - might benefit from higher
temperatures. However, in some areas rugged terrain and poor soil would
prevent these countries from compensating for reduced yields in today's more
productive areas. A warming of more than 2.5°C could reduce global food
supplies and contribute to higher food prices.
• Melting glaciers and the thermal expansion of sea water may raise sea
levels, threatening low-lying coastal areas and small islands. The global mean
sea level has already risen by around 10 to 20 centimetres during the past
century, and global warming is expected to cause a further rise of 9 to 88 cm
by the year 2100. The most vulnerable land would be the unprotected,
densely populated coastal regions of some of the world's poorest countries.
Bangladesh, whose coast is already prone to devastating floods, would be a
likely victim, as would many small island states such as the Maldives.
These scenarios are alarming enough to raise concern, but too uncertain
for easy decisions by governments. The picture is fuzzy. Some governments,
beleaguered by other problems and responsibilities and bills to pay, have
understandably been tempted to do nothing at all. Maybe the threat will go
away. Or someone else will deal with it. Maybe another giant asteroid will hit
the earth. Who knows?
9

• The Convention takes preliminary steps that clearly make sense for the
time being. Countries ratifying the Convention - called "Parties to the
Convention" in diplomatic jargon - agree to take climate change into account
in such matters as agriculture, energy, natural resources, and activities
involving sea-coasts. They agree to develop national programmes to slow
climate change. The Convention encourages them to share technology and to
cooperate in other ways to reduce greenhouse gas emissions, especially from
energy, transport, industry, agriculture, forestry, and waste management,
which together produce nearly all greenhouse gas emissions attributable to
human activity.
• The Convention encourages scientific research on climate change.
It calls for data gathering, research, and climate observation, and it creates a
"subsidiary body" for "scientific and technological advice" to help governments
decide what to do next. Each country that is a Party to the Convention must
also develop a greenhouse gas "inventory" listing its national sources (such as
factories and transport) and "sinks" (forests and other natural ecosystems that
absorb greenhouse gases from the atmosphere). These inventories must be
updated regularly and made public. The information they provide on which
activities emit how much of each gas is essential for monitoring changes in
emissions and determining the effects of measures taken to control emissions.
• It establishes a framework and a process for agreeing to specific
actions later. The diplomats who wrote the Framework Convention on Climate
Change saw it as a launching pad for potential further action in the future.
They recognized that it would not be possible in the year 1992 for the world's
governments to agree on a detailed blueprint for tackling climate change. But
by establishing a framework of general principles and institutions, and by
setting up a process through which governments meet regularly, they got
things started.
A key benefit of this approach is that it allowed countries to begin
discussing the issue even before they all fully agreed that it is, in fact, a
problem. Even skeptical countries have felt it is worthwhile participating. (Or,
to put it another way, they would have felt uneasy about being left out.) This
created legitimacy for the issue, and a sort of international peer pressure to
take the subject seriously.
The Convention is designed to allow countries to weaken or strengthen the
treaty in response to new scientific developments. For example, they can agree
to take more specific actions (such as reducing emissions of greenhouse gases
by a certain amount) by adopting "amendments" or "protocols" to the
Convention. This is what happened in 1997 with the adoption of the Kyoto
Protocol.
The treaty promotes action in spite of uncertainty on the basis of a recent
development in international law and diplomacy called the "precautionary
principle." Under traditional international law, an activity generally has not
been restricted or prohibited unless a direct causal link between the activity
and a particular damage can be shown. But many environmental problems,
such as damage to the ozone layer and pollution of the oceans, cannot be
confronted if final proof of cause and effect is required. In response, the
international community has gradually come to accept the precautionary
principle, under which activities that threaten serious or irreversible damage
can be restricted or even prohibited before there is absolute scientific certainty
about their effects.
1110

Countries in the early stages of industrialization - countries struggling hard
to give their citizens better lives - don't want these additional burdens.
Economic development is difficult enough already. If they agreed to cut back
on burning the fossil fuels that are the cheapest, most convenient, and most
useful for industry, how could they make any progress?
There are other injustices to the climate change problem. The countries to
suffer the most if the predicted consequences come about, if agricultural zones
shift or sea levels rise or rainfall patterns change, will probably be in the
developing world. These nations simply do not have the scientific or
economic resources, or the social safety nets, to cope with disruptions in
climate. Also, in many of these countries rapid population growth has pushed
many millions of people onto marginal land, the sort of land that can change
most drastically due to variations in climate.
• It puts the lion’s share of the responsibility for battling climate change -
and the lion’s share of the bill - on the rich countries. The Convention tries to
make sure that any sacrifices made in protecting our shared atmosphere will
be shared fairly among countries in accordance with their "common but
differentiated responsibilities and respective capabilities and their social and
economic conditions". It notes that the largest share of historical and current
emissions originates in developed countries. Its first basic principle is that
these countries should take the lead in combating climate change and its
adverse impacts. Specific commitments in the treaty relating to financial and
technological transfers apply only to very richest countries, essentially the
members of the Organization for Economic Cooperation and Development
(OECD). They agree to support climate change activities in developing
countries by providing financial support above and beyond any financial
assistance they already provide to these countries.
Specific commitments concerning efforts to limit greenhouse gas emissions
and enhance natural sinks apply to the OECD countries as well as to 12
"economies in transition" (Central and Eastern Europe and the former Soviet
Union). Under the Convention, the OECD and transition countries were
expected to try to return by the year 2000 to the greenhouse gas emission
levels they had in 1990 (as a group they succeeded).
If a giant asteroid hits the earth, that's nobody's fault. The same cannot be
said for global warming.
There is a fundamental unfairness to the climate change problem that
chafes at the already uneasy relations between the rich and poor nations of the
world. Countries with high standards of living are mostly (if unwittingly)
responsible for the rise in greenhouse gases. These early industrializers - Europe,
North America, Japan, and a few others - created their wealth in part by
pumping into the atmosphere vast amounts of greenhouse gases long before
the likely consequences were understood. Developing countries now fear
being told that they should curtail their own fledgling industrial activities - that
the atmosphere's safety margin is all used up.
Because energy-related emissions are the leading cause of climate change,
there will be growing pressure on all countries to reduce the amounts of coal
and oil they use. There also will be pressure (and incentives) to adopt
advanced technologies so that less damage is inflicted in the future. Buying
such technologies can be costly.
12 13

If the whole world starts consuming more and living
the good life, can the planet stand the strain?
As the human population continues to grow, the demands human beings
place on the environment increase. The demands are becoming all the greater
because these rapidly increasing numbers of people also want to live better
lives. More and better food, more and cleaner water, more electricity,
refrigerators, automobiles, houses and apartments, land on which to put
houses and apartments...
Already there are severe problems supplying enough fresh water to the
world's billions. Burgeoning populations are draining the water from rivers and
lakes, and vast underground aquifers are steadily being depleted. What will
people do when these natural "tanks" are empty? There are also problems
growing and distributing enough food - widespread hunger in many parts of
the world attests to that. There are other danger signals. The global fish harvest
has declined sharply; as large as the oceans are, the most valuable species
have been effectively fished out.
• The Convention recognises that poorer nations have a right to economic
development. It notes that the share of global emissions of greenhouse gases
originating in developing countries will grow as these countries expand their
industries to improve social and economic conditions for their citizens.
• It acknowledges the vulnerability of poorer countries to the effects of
climate change. One of the Convention's basic principles is that the specific
needs and circumstances of developing countries should be given "full
consideration" in any actions taken. This applies in particular to those whose
fragile ecosystems are highly vulnerable to the impacts of climate change. The
Convention also recognizes that states which depend on income from coal
and oil would face difficulties if energy demand changes.
1514

• The Convention calls for developing and sharing environmentally
sound technologies and know-how. Technology will clearly play a major role
in dealing with climate change. If we can find practical ways to use cleaner
sources of energy, such as solar power, we can reduce the consumption of coal
and oil. Technology can make industrial processes more efficient, water
purification more viable, and agriculture more productive for the same amount
of resources invested. Such technology must be made widely available - it must
somehow be shared by richer and more scientifically advanced countries with
poorer countries that have great need of it.
• The Convention emphasises the need to educate people about climate
change. Today's children and future generations must learn to look at the
world in a different way than it was looked at by most people during the 20th
century. This is both an old and a new idea. Many (but not all!) pre-industrial
cultures lived in balance with nature. Now scientific research is telling us to
do much the same thing. Economic development is no longer a case of "bigger
is better" - bigger cars, bigger houses, bigger harvests of fish, bigger doses of oil
and coal. We must no longer think of human progress as a matter of imposing
ourselves on the natural environment. The world - the climate and all living
things - is a closed system; what we do has consequences that eventually
come back to affect us. Tomorrow's children - and today's adults, for that
matter - will have to learn to think about the effects of their actions on the
climate. When they make decisions as members of governments and
businesses, and as they go about their private lives, they will have to take the
climate into account.
In other words, human behaviour will have to change - probably the
sooner the better. But such things are difficult to prescribe and predict. People
will need stronger signals and incentives if they are to do more for the good of
the global climate. That leads to...
Global warming is a particularly ominous example of humanity's
insatiable appetite for natural resources. During the last century we have dug
up and burned massive stores of coal, oil, and natural gas that took millions of
years to accumulate. Our ability to burn up fossil fuels at a rate that is much,
much faster than the rate at which they were created has upset the natural
balance of the carbon cycle. The threat of climate change arises because one
of the only ways the atmosphere - also a natural resource - can respond to the
vast quantities of carbon being liberated from beneath the earth's surface is to
warm up.
Meanwhile, human expectations are not tapering off. They are increasing.
The countries of the industrialized "North" have 20 per cent of the world's
people but use about 80 per cent of the world's resources. By global
standards, they live extremely well. It's nice living the good life, but if
everyone consumed as much as the North Americans and Western Europeans
consume - and billions of people aspire to do just that - there probably would
not be enough clean water and other vital natural resources to go around.
How will we meet these growing expectations when the world is already
under so much stress?
• It supports the concept of "sustainable development". Somehow,
mankind must learn how to alleviate poverty for huge and growing numbers of
people without destroying the natural environment on which all human life
depends. Somehow a way has to be found to develop economically in a
fashion that is sustainable over a long period of time. The buzzword for this
challenge among environmentalists and international bureaucrats is
"sustainable development". The trick will be to find methods for living well
while using critical natural resources at a rate no faster than that at which they
are replaced. Unfortunately, the international community is a lot farther along
in defining the problems posed by sustainable development than it is in
figuring out how to solve them.
1716

Emissions are still growing. Isn't it time to take some
serious action?
Three years after the Climate Change Convention was adopted at the Rio
Earth Summit, the Intergovernmental Panel on Climate Change (IPCC)
published its second major assessment of climate change research. Written
and reviewed by some 2,000 scientists and experts, the report was soon
famous for concluding that the climate may have already started responding to
past emissions. It also confirmed the availability of many cost-effective
strategies for reducing greenhouse gas emissions (the IPCC’s third assessment
was published in 2001).
Meanwhile, although emissions in some countries stabilized, emissions
levels continued to rise around the world. More and more people came to
accept that only a firm and binding commitment by developed countries to
reduce greenhouse gases could send a signal strong enough to convince
businesses, communities, and individuals to change their ways.
1918
The 1992 Convention was a good start. But as the years passed, and the
scientific evidence continued to accumulate, people naturally asked, "what's
next"?
In 1997, governments responded to growing public pressure by adopting
the Kyoto Protocol. A protocol is an international agreement that stands on its
own but is linked to an existing treaty. This means that the climate protocol
shares the concerns and principles set out in the climate convention. It then
builds on these by adding new commitments which are stronger and far more
complex and detailed than those in the Convention.
This complexity is a reflection of the enormous challenges posed by the
control of greenhouse gas emissions. It is also a result of the diverse political
and economic interests that had to be balanced in order to reach an
agreement. Billion-dollar industries will be reshaped; some will profit from the
transition to a climate-friendly economy, others will not.
Because the Kyoto Protocol will affect virtually all major sectors of the
economy, it is considered to be the most far-reaching agreement on
environment and sustainable development ever adopted. This is a sign that the
international community is willing to face reality and start taking concrete
actions to minimize the risk of climate change. The Protocol's negotiators were
able to take this important step forward only after facing up to some tough
questions.

20
Finally, there was the practical matter that the year 2000 was fast
approaching, and with it the Convention's non-binding "aim" for industrialized
countries - to return emissions to 1990 levels by the year 2000 - would expire.
Clearly, new steps were needed.
• It sets legally binding targets and timetables for cutting developed
country emissions. The Convention encouraged these countries to stabilize
emissions; the Protocol commits them to reducing their collective emissions by
at least 5%. Each country’s emissions levels will be calculated as an average of
the years 2008-2012; these five years are known as the first commitment
period. Governments must make "demonstrable progress" towards this goal by
the year 2005.
These arrangements will be periodically reviewed. The first review is likely
to take place in the middle of the first decade of the new century. At this time
the Parties will take "appropriate action" on the basis of the best available
scientific, technical, and socio-economic information. Talks on targets for the
second commitment period must start by 2005.
The Protocol will only become legally binding when at least 55 countries,
including developed countries accounting for at least 55% of developed
countries' 1990 CO2 emissions, have ratified it. This should happen some time
in 2003.
• The Protocol addresses the six main greenhouse gases. These gases are
to be combined in a "basket", so that reductions in each gas are credited
towards a single target number. This is complicated by the fact that, for
example, a kilo of methane has a stronger effect on the climate than does a
kilo of carbon dioxide. Cuts in individual gases are therefore translated into
"CO2 equivalents" that can be added up to produce one figure.
Cuts in the three major gases – carbon dioxide, methane, and nitrous
oxide - will be measured against a base year of 1990 (with exceptions for
some countries with economies in transition). Cuts in the three long-lived
industrial gases – hydrofluorocarbons (HFCs), perfluorocarbons (PFCs), and
sulphur hexafluoride (SF6 ) – can be measured against either a 1990 or 1995
baseline.
Carbon dioxide is by far the most important gas in the basket. It accounted
for over four fifths of total greenhouse gas emissions from developed countries
in 1995, with fuel combustion representing all but several percent of this amount.
Fortunately, CO2 emissions from fuel are relatively easy to measure and monitor.
Deforestation is the second largest source of carbon dioxide emissions in
developed countries. Under the Protocol, targets can be met in part by
improving the ability of forests and other natural sinks to absorb carbon
dioxide from the atmosphere. Calculating the amount absorbed, however, is
methodologically complex. Governments must still agree on a common
approach.
The second most important gas covered by the Protocol is methane.
Methane is released by rice cultivation, domesticated animals such as cattle,
and the disposal and treatment of garbage and human wastes. Methane
emissions are generally stable or declining in the developed countries and
their control does not seem to pose as great a challenge as carbon dioxide.
Nitrous oxide is emitted mostly as a result of fertilizer use. As with
methane, emissions from developed countries are stable or declining. Nitrous
oxide and methane emissions are also similar in being relatively difficult to
measure.
One major group of greenhouse gases that the Protocol does not cover is
chlorofluorocarbons. This is because CFCs are being phased out under the
1987 Montreal Protocol on Substances that Deplete the Ozone Layer. Thanks
to this agreement, atmospheric concentrations of many CFCs are stabilizing
and expected to decline over the coming decades.
However, the Protocol does address three long-lived and potent
greenhouse gases that, like CFCs, have been created by industry for
specialized applications. The use of HFCs and PFCs threatens to go up
dramatically in part because they are being adopted as ozone-safe
replacements for CFCs. Governments are now working to make sure that the
incentives and controls for ozone depletion and global warming are
compatible.
21

How can we make our behavior and our economies more
climate-friendly?
Minimizing greenhouse gas emissions will require policymakers to take
some tough decisions. Every time a subsidy is added or removed, and every
time a regulation or reform is put in place, somebody says "ouch". Even though
the economy as a whole stands to benefit from well-designed, market-oriented
policies for reducing emissions, action - or inaction - by government always
helps create winners and losers in the marketplace.
The challenge for policymakers is to design policies that fully engage the
energies of civil society. Their goal must be to open the floodgates of industrial
creativity. Experience shows that companies often respond rapidly and
positively to incentives and pressures. Given the right policy environment, the
business sector will roll out low-emissions technologies and services faster
than many now believe possible.
23
The third man-made gas, sulphur hexafluoride, is used as an electric
insulator, heat conductor, and freezing agent. Molecule for molecule, its
global warming potential is thought to be 23,900 times greater than that of
carbon dioxide.
• The Protocol recognizes that emissions cuts must be credible and
verifiable. Ensuring that governments comply with their targets will be
essential to the Protocol's success. Each country will need an effective national
system for estimating emissions and confirming reductions. Standardized
guidelines must be crafted to make figures comparable from one country to the
next and the whole process transparent.
The Protocol allows governments that cut emissions more than they are
required to by their national target to "bank" the "excess" as credits for future
commitment periods. But what happens if a country's emissions are higher
than what is permitted by its target? Non-compliance provisions still need to
be developed. Clearly, though, the best approach both politically and
environmentally will be to start by helping governments to comply rather than
emphasizing punitive or confrontational measures.
22

Schools, community groups, the media, families, and consumers also have
a crucial role to play. Individuals can make a real difference by changing their
habits and making thoughtful purchases and investments. If consumers are
convinced that the rules of the game are changing, they will start taking the
myriad small decisions that, when added together, can have a dramatic impact
on emissions.
If large segments of society are willing to make these changes, we can
expect an early transition to more energy-efficient, technologically innovative,
and environmentally sustainable societies. The trick is getting started.
• It highlights effective domestic policies and measures for reducing
emissions. National governments can build a fiscal and policy framework that
discourages emissions. They can phase out counter-productive subsidies on
carbon-intensive activities, and they can introduce energy-efficiency and other
regulatory standards that promote the best current and future technologies.
Taxes, tradable emissions permits, information programmes, and voluntary
programmes can all contribute.
Local and urban governments - which often have direct responsibility for
transport, housing, and other greenhouse gas-emitting sectors of the economy
- can also play a role. They can start designing and building better public
transport systems and creating incentives for people to use them rather than
private automobiles. They can tighten construction codes so that new houses
and office buildings will be heated or cooled with less fuel.
Meanwhile, industrial companies need to start shifting to new technologies
that use fossil fuels and raw materials more efficiently. Wherever possible they
should switch to renewable energy sources such as wind and solar power.
They should also redesign products such as refrigerators, automobiles, cement
mixes, and fertilizers so that they produce lower greenhouse gas emissions.
Farmers should look to technologies and methods that reduce the methane
emitted by livestock and rice fields. Individual citizens, too, must cut their use
of fossil fuels - take public transport more often, switch off the lights in empty
rooms - and be less wasteful of all natural resources.
The Protocol also flags the importance of conducting research into
innovative technologies, limiting methane emissions from waste management
and energy systems, and protecting forests and other carbon sinks.
• The Protocol encourages governments to work together. Policymakers
can learn from one other and share ideas and experiences. They may choose
to go further, coordinating national policies in order to have more impact in a
globalized marketplace. Governments should also consider the effects of their
climate policies on others, notably developing countries, and seek to minimize
any negative economic consequences.
24 25

How should we divide up the work - while sharing the
burden fairly?
The Climate Change Convention calls on the rich countries to take the
initiative in controlling emissions. In line with this, the Kyoto Protocol sets
emission targets for the industrialized countries only - although it also
recognizes that developing countries have a role to play.
Agreeing how to share the responsibility for cutting emissions amongst the
40 or so developed countries was a major challenge. Lumping all developed
countries into one big group risks ignoring the many differences between
them. Each country is unique, with its own mix of energy resources and price
levels, population density, regulatory traditions, and political culture.
For example, the countries of Western Europe tend to have lower per
capita emissions than do countries such as Australia, Canada, and the US.
Western Europe's emissions levels have generally stabilized since 1990 - the
base year for measuring emissions - while other developed countries have
seen their emissions rise. Japan made great strides in energy efficiency in the
26
1980s, while countries such as Norway and New Zealand have relatively low
emissions because they rely on hydropower or nuclear energy. Meanwhile, the
energy-intensive countries of Central and Eastern Europe and the former Soviet
Union have seen emissions fall dramatically since 1990 due to their transition
to market economies. These differing national profiles make it difficult to agree
on a one-size-fits-all solution.
• It assigns a national target to each country. In the end, it was not
possible to agree in Kyoto on a uniform target for all countries. The resulting
individual targets were not based on any rigorous or objective formula. Rather,
they were the outcome of political negotiation and compromise.
The overall 5% target for developed countries is to be met through cuts of
8% in the European Union (EU), Switzerland, and most Central and East
European states; 7% in the US (although the US has stated that it is no longer
committed to the Kyoto Protocol); and 6% in Canada, Hungary, Japan, and
Poland. New Zealand, Russia, and Ukraine are to stabilize their emissions,
while Norway may increase emissions by up to 1%, Australia by up to 8%,
and Iceland 10%.
The EU has made its own internal agreement to meet its 8% target by
distributing different rates to its member states, just as the entire developed
group's 5% target was shared out. These targets range from a 28% reduction
by Luxembourg and 21% cuts by Denmark and Germany to a 25% increase
by Greece and +27% for Portugal.
• The Protocol offers additional flexibility to the countries with
economies in transition. In particular, they have more leeway in choosing the
base year against which emissions reductions are to be measured. They also
do not share the commitment of the richer developed countries to provide
"new and additional financial resources" and to facilitate technology transfer
for developing country Parties.
27

• It also reconfirms the broader commitments of all countries - developed
and developing. Under the Convention, both developed and developing
countries agree to take measures to address emissions and adapt to future
climate change impacts; submit information on their national climate change
programmes and emissions levels; facilitate technology transfer; cooperate on
scientific and technical research;and promote public awareness, education,
and training. These commitments are reaffirmed in the Protocol, which also
sets out ways of advancing their implementation.
The issue of emissions targets for developing countries, and the broader
question of how commitments should evolve in the future given continuing
growth in global emissions, has generated a great deal of intense debate. A
proposal that the Protocol should establish a procedure whereby developing
countries could take on voluntary commitments to limit (that is, reduce the
rate of increase in) their emissions was not accepted in Kyoto. Many
developing countries resist formal commitments, even if voluntary, that would
put an upper limit on their emissions, noting that their per capita emissions are
still low compared to those of developed countries. Once developed countries
start to convincingly demonstrate that they are taking effective actions to
achieve their emissions targets, the debate on how new countries might
eventually be brought into the structure of specific commitments may be
revived.
This is in keeping with the step-by-step approach of the intergovernmental
climate regime. The Kyoto Protocol is not an end result, and can be
strengthened and built on in the future. What's more, although developing
countries are not currently subject to any specific timetables and targets, they
are expected to take measures to address climate change and to report on the
actions they are taking. There is a good deal of evidence that many developing
countries are indeed taking steps that should help their emissions grow at a
slower rate than their economic output. This is particularly true in the field of
energy.
I don't want to spend more money on this than is
absolutely necessary!
People are keen to combat climate change because they fear it may be
destructive and costly. At the same time, they naturally want to buy their
"climate insurance" at the lowest price possible.
Fortunately, the costs of climate change policies can be minimized
through "no regrets" strategies. Such strategies make economic and
environmental sense whether or not the world is moving towards rapid climate
change. For example, boosting energy efficiency not only reduces greenhouse
gas emissions but lowers the cost of energy, thus making industries and
countries more competitive in international markets; it also eases the health
and environmental costs of urban air pollution. At the same time, the
precautionary principle and the expected net damages from climate change
justify adopting policies that do entail some costs.
2928

Calculating the costs of climate change policies is not easy. How quickly
power plants and other infrastructure are replaced by newer and cleaner
equipment, how interest rate trends affect corporate planning and investment,
and the way businesses and consumers respond to climate change policies are
just a few of the variables to consider.
Costs can also vary from place to place. In general, the costs of improving
energy efficiency should be lower in countries that are the most energy
inefficient. Countries in the early stages of industrialization may offer cheaper
opportunities for installing modern environmentally friendly technologies than
do countries whose industrial plant is already developed. And so on.
• The Protocol innovates by giving Parties credit for reducing emissions
in other countries. It establishes three "mechanisms" for obtaining these
credits. The idea is that countries that find it particularly expensive to reduce
emissions at home can pay for cheaper emissions cuts elsewhere. The global
economic efficiency of reducing emissions is increased while the overall 5%
reduction target is still met. The Protocol stipulates, however, that credit for
making reductions elsewhere must be supplementary to domestic emissions
cuts.
Governments must still decide just how the three mechanisms for doing
this will function. The rules they adopt will strongly influence the costs of
meeting emissions targets. They will also determine the environmental
credibility of the mechanisms - that is, their ability to contribute to the
Protocol's aims rather than opening up "loopholes" in emissions commitments.
• An emissions trading regime will allow industrialized countries to buy
and sell emissions credits amongst themselves. Countries that limit or reduce
emissions more than is required by their agreed target will be able to sell the
excess emissions credits to countries that find it more difficult or more
expensive to meet their own targets. The rules, however, have not yet been
decided on.
Some observers are concerned that the Kyoto targets of some countries are
so low that they can be met with minimal effort. These countries could then
sell large quantities of emission credits (known as "hot air"), reducing pressure
on other industrialized countries to make domestic cuts. Governments are
debating the best way to ensure that emissions trading does not undermine
incentives for countries to cut their own domestic emissions.
• Joint implementation (JI) projects will offer "emissions reduction units"
for financing projects in other developed countries. A joint implementation
project could work like this: Country A faces high costs for reducing domestic
emissions, so it invests in low-emissions technologies for a new power plant in
Country B (very likely an economy in transition). Country A gets credit for
reducing emissions (at a lower cost that it could domestically), Country B
receives foreign investment and advanced technologies, and global
greenhouse gas emissions are reduced: a "win-win-win" scenario.
Not only governments, but businesses and other private organizations will
be able to participate directly in these projects. Some aspects of this approach
have already been tested under the Convention through a voluntary
programme for "Activities Implemented Jointly". Reporting rules, a monitoring
system, institutions, and project guidelines must still be adopted. Not only
must this infrastructure establish the system's credibility, but it must ensure that
JI projects transfer appropriate and current technology, avoid adverse social
and environmental impacts, and avoid distorting the local market.
• A Clean Development Mechanism will provide credit for financing
emissions-reducing or emissions-avoiding projects in developing countries.
This promises to be an important new avenue through which governments and
private corporations will transfer clean technologies and promote sustainable
development. Credit will be earned in the form of "certified emissions
reductions".
Whereas joint implementation and emissions trading merely shift around
the pieces of the industrial countries' overall 5% target, the CDM involves
emissions in developing countries (which do not have targets). This in effect
increases the overall emissions cap. Verification is therefore particularly
important for this mechanism.
3130

The Protocol already details some of the ground rules. The CDM will be
governed by the Parties through an Executive Board, and reductions will be
certified by one or more independent organizations. To be certified, a deal
must be approved by all involved parties, demonstrate a measurable and long-
term ability to reduce emissions, and promise reductions that would be
additional to any that would otherwise occur. A share of the proceeds from
CDM projects will be used to cover administrative expenses and to help the
most vulnerable developing countries meet the costs of adapting to climate
change impacts. Again, the operational guidelines must still be worked out.
The 21st century and beyond
Climate change would have lasting consequences. One giant asteroid
came along 65 million years ago, and that was it for the dinosaurs.
In facing up to man-made climate change, human beings are going to have
to think in terms of decades and centuries. The job is just beginning. Many of
the effects of climate shifts will not be apparent for two or three generations. In
the future, everyone may be hearing about and living with this problem.
The Framework Convention takes this into account. It establishes
institutions to support efforts to carry out long-term commitments and to
monitor long-term efforts to minimize and adjust to climate change. The
Conference of the Parties, in which all states that have ratified the treaty are
represented, is the Convention's supreme body. It met for the first time in 1995
and will continue to meet on a regular basis to promote and review the
implementation of the Convention. The Conference of the Parties is assisted by
two subsidiary bodies (or committees), one for scientific and technological
advice and the other for implementation. It can establish other bodies as well,
whether temporary or permanent, to help it with its work.
It can also strengthen the Convention, as it did in Kyoto in 1997. The
Protocol's five per cent cut may seem a modest start, but given the rise in
emissions that would otherwise be expected and remember that emissions in a
number of developed countries have risen steadily since the 1990 base year
many countries are going to have to make a significant effort to meet their
commitment.
The Kyoto Protocol makes an important promise: to reduce greenhouse
gases in developed countries by the end of the first decade of the new century.
It should be judged a success if it arrests and reverses the 200-year trend of
rising emissions in the industrialized world and hastens the transition to a
climate-friendly global economy.
3332

Keygreenhousegasesaffectedbyhumanactivities
CO2CH4N2OCHC-11HFC-23CF4
(Carbon(Methane)(Nitrous(Chlorofluoro-(Hydrofluoro-(Perfluoro-
Dioxide)Oxide)carbon11)carbon-23)methane)
Pre-industrialconcentration~280ppm~700ppb~270ppbzerozero40ppt
1998concentration365ppm1745ppb314ppb268ppt14ppt80ppt
Rateofincreasechange*1.5ppm/yra7.0ppb/yra0.8ppb/yr-1.4ppt/yr0.55ppt/yr1ppt/yr
Lifetime(years)5-200yrc12yrd114yrd45yr260yr>50.000yr
Notes:
aRatehasfluctuatedbetween0.9ppm/yrand2.8ppm/yrforCO2andbetween0and13ppb/yrforCH4overtheperiod1990to1999.
bRateiscalculatedovertheperiod1990to1999.
cNosinglelifetimecanbedefinedforCO2becauseofthedifferentratesofuptakebydifferentremovalprocesses.
dThislifetimehasbeendefinedasan“adjustmenttime”thattakesintoaccounttheindirecteffectofthegasonitsownresidencetime.
Source:“Climate2001,TheScientificBasis,TechnicalSummaryoftheWorkingGroupIReport”,p.38.

For more information, please contact:
United Nations Environment Programme
Information Unit for Conventions
International Environment House, Geneva
1219 Châtelaine, Switzerland
Tel. +41-22-917-8244/8196
Fax.: +41-22-797-3464
iuc@unep.ch, www.unep.ch/conventions/
Climate Change Secretariat
Haus Carstenjan
PO Box 260124
D-53153 Bonn, Germany
secretariat@unfccc.int, www.unfccc.int
Printed in France
GE.02-01877/E-September 2002

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