BACKGROUNDER
Basic Facts and Data on the Science
and Politics of Ozone Protection
1.
The Ozone Layer
Ozone molecules (O3) consist of three oxygen atoms. This
poisonous gas is extremely rare in the atmosphere, representing just three out
of every 10 million molecules. Ninety per cent of ozone exists in the upper
atmosphere, or stratosphere, between 10 and 50 km (6‑30 miles) above the
earth. Ozone at ground‑level, at the bottom of the troposphere, is a harmful
pollutant resulting from automobile exhausts and other sources.
Figure 1 - Ozone Distribution in the Atmosphere
The ozone layer absorbs most of the harmful ultraviolet‑B radiation
from the sun. It also completely screens out lethal UV‑C radiation.
The ozone shield is thus essential to life as we know it. Depleting the ozone
layer allows more UV‑B to reach the earth. More UV‑B means more
melanoma and non‑melanoma skin cancers, more eye cataracts, weakened immune
systems, reduced plant yields, damage to ocean eco‑systems and reduced
fishing yields, adverse effects on animals, and more damage to plastics.
Scientific concern started in 1970 when Prof. Paul Crutzen pointed out
the possibility that nitrogen oxides from fertilizers and supersonic aircraft
might deplete the ozone layer. In 1974, Professors F. Sherwood Rowland and Mario
J. Molina recognized that when CFCs finally break apart in the atmosphere and
release chlorine atoms they cause ozone depletion. Bromine atoms released by
halons have the same effect. The three scientists received the Nobel Prize for
Chemistry in 1995 for their pioneering work.
The ozone layer over the Antarctic has steadily weakened since measurements
started in the early 1980s. The problem is worst over this part of the globe
due to the extremely cold atmosphere and the presence of polar stratospheric
clouds. The land area under the ozone‑depleted atmosphere increased steadily
to more than 20 million sq km in the early 1990s and has varied between 20 and
29 million sq. km since then. In 2000, the area of the ozone hole reached a
record 29 million sq. kilometers on 12 September 2000. Although
it was the largest and the deepest ozone hole on record for the month of September,
it dissipated early in October, the earliest since 1991. The lowest value recorded
at the South Pole was 86 DU on 12
October 1993. This year, the area of the ozone hole has been about
25 million sq. km. While no hole has appeared elsewhere, the Arctic spring has
seen the ozone layer over the North Pole thin by up to 30%, while the depletion
over Europe and other high latitudes varies between 5%
and 30%.
Figure 2 - Measurements of Ozone and Reactive Chlorine from
a Flight Into the Antarctic Ozone Hole, 1987
2.
Adopting and Ratifying the Vienna
Convention, the Montreal Protocol,
and Amendments to the Protocol
The issue of ozone depletion was first discussed by the Governing Council
of the United Nations Environment Programme (UNEP) in 1976. A meeting of
experts on the ozone layer was convened in 1977, after which UNEP and the World
Meteorological Organization (WMO) set up the Coordinating Committee of the Ozone
Layer (CCOL) to periodically assess ozone depletion. Inter‑governmental
negotiations for an international agreement to phase out ozone‑depleting
substances started in 1981 and concluded with the adoption of the Vienna Convention
for the Protection of the Ozone Layer in March 1985.
The 1985 Vienna
Convention encourages intergovernmental cooperation on research, systematic
observation of the ozone layer, monitoring of CFC production, and the exchange
of information. The Convention commits its Parties to take general measures
to protect human health and the environment against human activities that modify
the ozone layer. The Vienna Convention is a framework agreement and does not
contain legally binding controls or targets.
The Montreal Protocol
on Substances that Deplete the Ozone Layer was adopted in September 1987. Following
the discovery of the Antarctic ozone hole in late 1985, governments recognized
the need for stronger measures to reduce the production and consumption of a
number of CFCs (CFC‑11, 12, 113, 114, and 115) and several Halons (1211,
1301, 2402). The Protocol was designed so that the phase‑out schedules
could be revised on the basis of periodic scientific and technological assessments.
Following such assessments, the Protocol was adjusted to accelerate the phase‑out
schedules in London in 1990, Copenhagen
in 1992, Vienna in 1995, Montreal
in 1997, and Beijing in 1999. It
has also been amended to introduce other kinds of control measures and to add
new controlled substances to the list; the 1990 London Amendment included additional
CFCs (CFC‑13, 111, 112, 211, 212, 213, 214, 215, 216, 217) and the two
solvents (carbon tetrachloride and methyl chloroform), while the 1992 Copenhagen
Amendment added methyl bromide, HBFCs, and HCFCs.
The Montreal Amendment of 1997 finalized the schedules for phasing out methyl
bromide. The Beijing Amendment of 1999 included Bromochloromethane for immediate
phase out; it also introduced production controls on HCFCs as well as controls
on trade with non-Parties.
Governments are not legally bound until they ratify the Protocol as well
as the Amendments. Unfortunately, while most governments have ratified the
Protocol, ratification of the amendments and their stronger control measures
lag behind. As of 2 July 2003, the Ozone Agreements had
been ratified by countries as depicted in the figure 3 chart:
Figure 3 - Ratification Status of the Montreal
Protocol and its Amendments as of July 2003.
3.
The Chemicals And Their Phase‑Out Schedules
Ninety‑six (96) chemicals are presently controlled by the Montreal
Protocol, including:
· Halo‑carbons,
notably chlorofluorocarbons (CFCs) and Halons. CFCs
were discovered in 1928 and were considered wonder gases because they are long‑lived,
non‑toxic, non‑corrosive, and non‑flammable. They are also
versatile and from the 1960s were increasingly used in refrigerators, air conditioners,
spray cans, solvents, foams, and other applications. CFC‑11 remains in
the atmosphere for 50 years, CFC‑12 for 102 years, and CFC‑115 for
1,700. Halon 1301 is used primarily in fire extinguishers and has an atmospheric
lifetime of 65 years.
· Carbon tetrachloride
is used as a solvent and takes about 42 years to break down in the atmosphere.
· Methyl chloroform
(1,1,1‑trichloroethane) is also used as a solvent and takes about 5.4
years to break down.
· Hydrobromofluorocarbons
(HBFCs) are not widely used, but they have been included under the Protocol
to prevent any new uses.
· Hydrochlorofluorocarbons
(HCFCs) were developed as the first major replacement for CFCs. While
much less destructive than CFCs, HCFCs also contribute to ozone depletion. They
have an atmospheric lifetime of about 1.4 to 19.5 years.
· Methyl bromide (CH3Br)
is used as a fumigant for high‑value crops, pest control, and quarantine
treatment of agricultural commodities awaiting export. Total world annual consumption
is about 70,000 tonnes, most of it in the industrialized countries. It takes
about 0.7 years to break down.
· Bromochloromethane
(BCM), a new ozone-depleting substance that some companies sought to
introduce into the market in 1998, has been targeted by the 1999 Amendment for
immediate phase-out to prevent its use.
· The Parties are considering
measures to prevent the marketing of new ozone-depleting substances not so far
covered by the Protocol.
The phase‑out schedules for developed countries are as follows:
Ø Phase out Halons by 1994;
Ø Phase out CFCs, carbon tetrachloride, methyl
chloroform, and HBFCs by 1996;
Ø Reduce methyl bromide by 25% by 1999, 50% by
2001, 70% by 2003, and phase out by 2005; and
Ø Reduce HCFCs by 35% by 2004, 65% by 2010, 90%
by 2015, and 99.5% by 2020, with 0.5% permitted for maintenance purposes only
until 2030.
Ø Phase out HBFCs by 1996 and phase out BCM immediately.
Developing countries have a grace period before they must start their phase‑out
schedules. This reflects the recognition that developed countries are responsible
for the bulk of total emissions into the atmosphere and that they have more
financial and technological resources for adopting replacements. The developing
country schedules are as follows:
Ø Phase out HBFCs by 1996 and phase out BCM immediately;
Ø Freeze CFCs, Halons and carbon tetrachloride
at average 1995‑97 levels by 1
July 1999, reduce by 50% by 2005, 85% by 2007, and phase out completely
by 2010;
Ø Freeze methyl chloroform by 2003 at average
1998‑2000 levels, reduce by 30% by 2005, 70% by 2010, and phase out by
2015;
Ø Freeze methyl bromide by 2002 at average 1995‑98
levels, reduce by 20% by 2005, and phase out by 2015; and
Ø Freeze HCFCs by 2016 at 2015 levels and phase
out by 2040.
The phase‑out schedules cover both the production and the consumption
of the target substances. However, even after phase out both developed and
developing countries are permitted to produce limited quantities in order to
meet the essential uses for which no alternatives have yet been identified,
e.g. the use of CFCs in metered dose inhalers for asthma. Production is defined
as total production minus amounts destroyed or used as chemical feedstock. Consumption
is defined as production plus imports minus exports. Trade in recycled and used
chemicals is not included in the calculation of consumption in order to encourage
recovery, reclamation and recycling. 4. What Have Been
The Results So Far?
Without the Protocol, by the year 2050 ozone depletion would have risen
to at least 50% in the northern hemisphere's mid latitudes and 70% in the southern
mid latitudes, about 10 times worse than current levels. The result would
have been a doubling of UV‑B radiation reaching the earth in the northern
mid latitudes and a quadrupling in the south. The amount of ozone‑depleting
chemicals in the atmosphere would have been five times greater. The implications
of this would have been horrendous: 19 million more cases of non‑melanoma
cancer, 1.5 million cases of melanoma cancer, and 130 million more cases of
eye cataracts.
In 1986 the total consumption of CFCs world‑wide was about 1.1 million
ODP tonnes; by 2001 this had come down to about 110,000 tonnes. It has been
calculated that without the Montreal Protocol global consumption would have
reached about 3 million tonnes in the year 2010 and 8 million tonnes in 2060,
resulting in a 50% depletion of the ozone layer by 2035.
The bulk of the 1986 total, or about 0.9 million ODP tonnes, was consumed in
developed countries, but by 2001 these countries consumed just about 7,000 tonnes,
including for exemptions approved by the Parties. The developing countries have
reduced their CFC consumption by about 15% from 1986 to 2001.
Three of the 130 developing countries (Brazil,
China and Republic
of Korea), accounted for about 46%
of this group's consumption for 2001, while 8 more countries (Argentina,
India, Indonesia,
Iran, Mexico,
Nigeria, Thailand
and Venezuela),
accounted for a further 28% consumption.
Figure 5 - Worldwide Production and Consumption of CFCs
Scientists predict that ozone depletion will reach its worst point during
the next few years and then gradually decline until the ozone layer returns
to normal around 2050, assuming that the Montreal Protocol is fully implemented.
The ozone layer is currently in its most vulnerable state. Despite declining
CFC emissions, stratospheric concentrations are still increasing
(although they are declining in the lower atmosphere) because long‑lived
CFCs emitted in earlier years continue to rise to the stratosphere.
The atmospheric abundance of certain CFCs (notably CFC‑11 and CFC‑113),
carbon tetrachloride, and methyl chloroform is declining. The abundance of most
of the halons continues to increase. Concentrations of HCFCs and HFCs are, of
course, increasing, since they are used as substitutes for the CFCs that are
being phased out.
The success of ozone protection has been possible because science and industry
have been able to develop and commercialize alternatives to ozone‑depleting
chemicals. Developed countries ended the use of CFCs faster and with less
cost than was originally anticipated. Substitutes have proved particularly important
in electronics. The foam‑blowing sector has made use of water, carbon‑dioxide,
and hydrocarbons, as well as HCFCs. The refrigeration and air‑conditioning
sector has largely used HCFCs as alternatives, but new equipment is increasingly
using replacements with zero ozone‑depleting potential, including hydrofluorocarbons
(HFCs), ammonia, and hydrocarbons.
HFCs have a high global warming potential and have been included in the
basket of greenhouse gases controlled by the Kyoto
Protocol of the Convention on Climate Change. Countries are now trying to
minimise their emissions of HFCs.
Consumers are recycling existing Halons to gain time for developing substitutes
for fire fighting. Other extinguishing agents such as carbon dioxide, water,
foam, and dry powder are now widely used. Alternative approaches, such as good
fire prevention practices, use of fire‑resistant materials, and appropriate
designs for buildings have significantly reduced the need for Halon systems,
and total phase‑out was achieved smoothly by 1994.
Countries are recovering and recycling CFCs from obsolete
equipment and using it for maintenance of existing equipment.
Industrialized countries are concentrating their phase‑out efforts
on HCFCs and methyl bromide. They are trying to ensure that HCFCs are used
only as direct replacements where other more environmentally suitable alternatives
are not available. HCFCs were critical for meeting the early CFC phase‑out
goals but are generally considered undesirable for most new equipment because
they do have some ozone‑depleting potential and ozone-safe alternatives
are available for most applications.
5.
A summary of the 2002 findings of the Assessment Panels
Science:
· The Montreal
Protocol is working. However, even with full compliance of the Montreal Protocol
by all Parties, the ozone layer will remain particularly vulnerable during the
next decade or so.
· The total
combined effective abundance of ozone-depleting compounds in the lower atmosphere
continues to decline slowly from the peak that occurred in 1992-1994. Total
chlorine is declining, while bromine from industrial halons is still increasing,
albeit at a slower rate than was occurring previously. The abundances of HCFCs
in the lower atmosphere are increasing. ·
Observations in the stratosphere indicate that the total chlorine abundance
is at or near a peak, while bromine abundances are probably still increasing.
· Springtime Antarctic ozone
depletion due to halogens has been large throughout the last decade. In some
recent cold Arctic winters during the last decade, maximum total column ozone
losses due to halogens have reached 30%. Ozone remains depleted in the midlatitudes
of both hemispheres. · The global
ozone layer recovery has been linked mainly to decreasing chlorine and bromine
loading. A return to pre-1980 total column ozone amounts in the Antarctic is
expected by the middle of this century. Although Arctic ozone depletion is
difficult to predict, a future Arctic polar ozone hole similar to that of the
Antarctic appears unlikely. ·
Very short-lived organic chlorine-, bromine-, and iodine-containing gases have
the potential to deplete stratospheric ozone. Quantitative estimation of their
ozone depleting potentials is challenging but they could vary up to 0.1. The
impact of very short-lived compounds can be significant if their emissions are
large.
· Other factors
such as climate change and changes in atmospheric transport are likely to influence
the recovery of the ozone layer. New research has begun to explore the coupling
between climate change and the recovery of the ozone layer.
Environmental Effects:
· New studies
continue to confirm the adverse effects of UV-B radiation on the eyes, skin,
and immune system, including cortical cataract and skin cancer.
· Phase-out
of the ozone-depleting chemical, methyl bromide, may lead to increased use and
numbers of other pesticides which may lead to additional health risks.
· Interactions
between global climate change and ozone depletion are likely to influence the
risk of adverse effects of UV-B radiation on health.
· Interaction
of ultraviolet radiation with other global climate change factors may affect
many ecosystem processes such as plant biomass production, plant consumption
by herbivores including insects, disease incidence of plants and animals, and
changes in species abundance and composition.
· Recent results
continue to confirm the general consensus that solar UV negatively affects aquatic
organisms (zooplankton, as well as larval stages of primary and secondary consumers).
· In addition
to increasing solar UV-B radiation, aquatic ecosystems are confronted with other
environmental stress factors including increased nutrient input, pollution,
acidification and global climate change. ·
Global warming and enhanced UV-B radiation interact to affect a range of biogeochemical
processes including microbial activity, nutrient cycling, and greenhouse gas
emissions from soils.
· Interactions
between ozone depletion and climate change will have an impact on tropospheric
hydroxyl (OH) radical concentration, the “cleaning” agent of the troposphere.
· Climate change is likely to
modify the rates of UV-induced degradation of natural and synthetic materials.
Technology and Economics:
· The remaining
7,000 ODP tonnes of CFCs used annually in MDIs for asthma/COPD can be phased
out. The timing is difficult to predict, but it depends on the availability
of affordable alternatives and the adoption and effectiveness of transition
strategies by Parties.
· In the last
four years there has been a substantial phase-out of CFCs in non-MDI aerosols
and a complete phase-out for non-MDI aerosols is achievable. There are difficulties
including the availability of hydrocarbon aerosol propellants, the conversion
of small CFC users, and also the conversion of non-MDI pharmaceutical aerosols.
· Most miscellaneous uses have
been phased out, whilst some laboratory uses still remain under a global exemption.
· The use of CFCs in foams has
been reduced by over 90% since its peak in 1988 and HCFC use is also in decline
from its peak in 2000. The phase-out of ODS in the foam sector has forced the
industry to innovate faster than ever before. The first transition technology
led to the introduction of substances such as HCFCs as well as the increasing
use of hydrocarbons and other non-ODSs. Attention is now on the emerging HFC-based
technologies as well as the further optimisation and use of hydrocarbon and
CO2 technologies.
· Halon fire
extinguishants are no longer necessary in virtually any new installations, with
the possible exceptions of engine nacelles and cargo compartments on commercial
aircraft and crew compartments of combat vehicles. The very high cost of replacing
many existing halon systems with substitutes, replacements or other alternative
fire protection measures continues to be a major impediment to eliminating continued
use of halons.
· Production
of methyl bromide (MB) for controlled uses was reported to be about 62,000 metric
tonnes in 1998; it was reduced to at least 49,000 tonnes in 1999 and at least
46,000 tonnes in 2000. The decline in total global consumption of MB is attributed
largely to reductions for soil fumigation. No existing technical alternatives
for about 3,200 metric tonnes of MB per annum used for non-QPS treatments could
be found yet. · With two exceptions
(control of ginseng root rot and stabilisation of high-moisture fresh dates),
the completed demonstration projects identified one or more alternatives comparable
to MB in their effectiveness in the control of targeted pests and diseases and
demonstrated that a similar range of alternatives to those in developed countries
can be successfully adopted. ·
In the last decade, the refrigeration, air conditioning and heat pump industry
made tremendous technical progress in phasing out CFCs and, in several applications,
HCFCs as well. The mobile air conditioning and the domestic refrigeration industries
have shifted rapidly from CFC-12 to non-ODS refrigerants. Other applications,
such as chillers and commercial refrigeration, have shifted from CFCs to HCFCs,
HFCs or other fluids. Worldwide, a significant amount of installed refrigeration
equipment still uses CFCs and HCFCs. As a consequence, service demand for CFCs
and HCFCs remains high. · There
is much left to be achieved in the Solvents Sector. Effort is still required
to phase out ODS solvents in developing countries, and especially the small-
and medium-sized users. In particular, there is concern about the use of carbon
tetrachloride (CTC) for solvent applications by both large and small enterprises
in some countries.
6.
The Multilateral Fund of the Montreal
Protocol and the GEF
The Multilateral Fund of the Montreal
Protocol is part of the financial mechanism established under the Protocol in
June 1990. It pays the agreed incremental costs incurred by developing countries
in phasing out their consumption and production of ozone‑depleting substances.
It is administered by an Executive Committee of seven developed and seven developing
countries chosen by the Parties every year. The Fund's allocation was $240 million
for 1991‑93, $455 million for 1994‑96, $465 million for 1996‑99
and $440 million for 2000‑2. The replenishment for the three‑year
period of 2003‑5 was fixed at $474 million by the Parties at their Rome
meeting in November 2002. The Multilateral Fund has thus far disbursed over
1.4 billion dollars for capacity building and projects to phase out CFCs.
Figure 6 - Multilateral Ozone Fund: Cumulative Funds Approved
and CFC Tonnes Phased Out.
The Global Environment Facility (GEF) was established by the world community
to help developing countries deal with ozone depletion, climate change, biodiversity,
and international waters. GEF supports projects and activities for phasing‑out
ozone‑depleting substances in countries with economies in transition,
as most of these Central and East European countries are not eligible for Multilateral
Fund assistance. GEF approved over US$ 160 million to assist the following 17
countries in the phase-out of Annex A and B substances: Azerbaijan, Belarus,
Bulgaria, Czech Republic, Estonia, Hungary, Kazakhstan, Latvia, Lithuania, Poland,
Russian Federation, Slovakia, Slovenia, Tajikistan, Turkmenistan, Ukraine and
Uzbekistan. Additional funds of US$ 60 million have been ear-marked by GEF to
assist CEIT countries with the phase-out of HCFCs and Methyl Bromide.
7.
Implementing Agencies of the Multilateral Fund and GEF
The UN Environment Programme, the UN Development Programme and the World Bank
implement the programmes of the Fund and the GEF in developing countries and
in countries with economies in transition. In addition, the UN Industrial Development
Organization was included later as an additional implementing agency of the
Fund.
UNEP is responsible for information exchange, institutional strengthening,
networking and preparation of country programmes. It has assisted over 100 developing
countries as well as countries that were formerly part of the Soviet
Union.
UNDP, UNIDO and the World Bank are responsible for technical assistance and
investment projects for phasing out ozone-depleting substances in all countries
receiving assistance.
8.
The Remaining Challenges
The Protocol has been hailed as an extraordinary success so far, but there
is no room for complacency because:
Ratification is incomplete.
Eleven countries have not yet ratified the ozone treaties, and many more have
not yet ratified the London, Copenhagen,
Montreal and Beijing Amendments.
Some countries with economies in transition are having difficulty complying
with the Montreal
Protocol.
This is due to the economic recession and political transition since 1989. The
Russian Federation
and a few other countries admitted in 1996 that they would be unable to follow
the phase‑out time‑table for CFCs. Many have, however, managed to
complete the phase‑out by the year 2002. The Parties asked the GEF to
provide this assistance, and it has thus far allocated over $160 million to
these countries. In addition, the World Bank's Special Initiative raised $19
million from Austria,
Denmark, Finland,
Germany, Italy,
Japan, Norway,
Sweden, UK
and US to close down the production of CFCs and Halons in the Russian
Federation by the year 2000. The GEF has approved
a further $60 million to assist these Parties with the phase-out of HCFCs and
Methyl Bromide.
Illegal trade has increased.
Although all new CFCs are now banned in industrialized countries, millions of
CFC‑dependent refrigerators, automobile air conditioners, and other equipment
are still in service. Alternatives are available to service this equipment,
but they can be more expensive. Recycled CFCs may be used to maintain existing
equipment, but it is difficult to distinguish between new and recycled CFCs.
In addition, while most consumption is forbidden, industrialized countries still
produce some CFCs in order to meet their own essential uses and to supply developing
countries, as permitted by the Protocol. In the US,
CFCs are heavily taxed and the market price is high. As a result, some traders
illegally sell perhaps 20,000 tonnes of new CFCs in the industrialized countries
every year in the guise of recycled substances or as exports to developing countries.
Smugglers are subject to imprisonment and heavy fines, and national licensing
systems are being established to better track imports and exports.
The potential for methyl bromide to be adopted in more applications and
by more countries is worrying.
Some countries imposed controls on this chemical because of its toxicity
even before the concern about its ozone depletion potential first arose. However,
since many countries have not yet ratified the 1992 Copenhagen Amendment which
introduced controls on methyl bromide, there is a risk that consumption could
spread to more countries and to more uses.
Atmospheric concentrations of Halons continue to increase even though production
ended in 1994.
This is because Halons in existing fire‑fighting equipment get emitted
whenever there is a fire. This is a concern because the bromine contained in
Halons is 50 times more efficient than the chlorine in CFCs in depleting ozone.
An expert panel is exploring the implications of de‑commissioning existing
Halons systems and destroying the Halons they contain.
Meeting the phase-out schedules by the developing countries!
With the arrival of the freeze on CFC production and consumption for the
Article 5 Parties, the grace period granted to them by the Montreal Protocol
has now ended. The Article 5 Parties have entered the “compliance” period in
which they will have to achieve specific reductions in the national production
and consumption of CFCs.
Figure 7 - Measured Atmospheric Concentration of Halons at
Cape Grim, Tasmania.
Developing countries must implement their phase out of CFCs, Halons and
carbon tetrachloride according to the schedule. Asian countries, in particular,
have been increasing their consumption due to their high rates of economic growth
and must now stabilize this consumption and begin reversing it. While consumption
levels in the developed countries – which had been much higher on both a per-capita
and a national basis – have been virtually phased out, the Montreal Protocol
can only succeed if the developing countries – with 80% of world population
– phase out these substances despite their growing economies. The Multilateral
Fund will play an essential role in ensuring that this happens.
A large number of used CFC‑based refrigerators are being exported
to developing countries by countries that have phased out CFCs. These sales
could make the future CFC phase out by developing countries more difficult by
stimulating a large demand for CFCs to maintain this equipment.
CFCs are being replaced by HFCs, which have a large global warming potential.
The Kyoto Protocol on climate change has included HFCs in the basket of six
gases whose emissions are to be reduced by the industrialised countries. Are
the two global protocols sending confusing signals? Does the Kyoto Protocol
hinder the implementation of the Montreal Protocol? The Parties to the Montreal
Protocol as well as the Parties to the Climate Change Convention now have the
reports of their scientific and technical panels on how to minimise the emissions
of HFCs. Implementation of the panels’ recommendations by governments is important.
Figure 8 - Worldwide Production of CFCs, HCFCs and HFCs
9.
Lessons of the Montreal Protocol
The Montreal Protocol
offers many lessons that could be applied to solving other global environmental
issues:
· Adhere to the "precautionary
principle" because waiting for complete scientific proof can delay action
to the point where the damage will become irreversible.
· Send consistent and credible
signals to industry (e.g. by adopting legally binding phase‑out schedules)
so that they have an incentive to develop new and cost‑effective alternative
technologies.
· Ensure that improved scientific
understanding can be incorporated quickly into decisions about the provisions
of a treaty.
· Promote universal participation
by recognizing the "common but differentiated responsibility" of developing
and developed countries and ensuring the necessary financial and technological
support to developing countries.
· Control measures should be
based on an integrated assessment of science, economics, and technology.
10. Note to Journalists
This backgrounder was updated on 2
July, 2003. Official documents and other information is available
via the Internet at http://www.unep.org/ozone or at http://www.unep.ch/ozone.
The Ozone Secretariat is based in Nairobi.
For interviews or additional information, contact:
¢ Nick Nuttall: Tel. (+254 20) 623084, Fax. (+254 20) 623692, e mail:
Nick.Nuttall@unep.org; or
¢ Michael Williams: Tel. (+41 22) 917 8242, fax (+41 22) 797 3464, e mail:
mwilliams@unep.ch; or
¢ Eric Falt: Tel. (+1 212) 963 8098, fax (+1 212) 963 8193, e mail: Eric.Falt@unep.org.
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