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temperature has increased by about half a degree centigrade over the last century; the last few decades have been the hottest this century; and this year may be the hottest on record.

The atmospheric concentrations of greenhouse gases have increased since the beginning of the preindustrial era due to human activities; carbon dioxide by about 30%, methane by more than a factor of two, and nitrous oxide by about 15%. Their concentrations are higher now than at any time during the last 160,000 years, the period for which there is reliable ice-core data, and probably significantly longer. In addition, the atmospheric concentrations of sulfate aerosols have also increased this century. Greenhouse gases tend to warm the atmosphere and, in some regions, aerosols tend to cool the atmosphere.

Theoretical models that take into account the observed increases in the atmospheric concentrations of greenhouse gases and sulfate aerosols simulate quite well the observed changes in both surface temperature and vertical temperature distribution. This suggests that human activities are implicated in the observed changes in the Earth's climate.

Based on the estimated range of climate sensitivities and plausible ranges of greenhouse gas and sulfur dioxide emissions (IPCC IS 92), climate models project that the global mean surface temperature could increase by 1 to 3.5oC by 2100. These projected global-average temperature changes would be greater than recent natural fluctuations, would also occur at a rate significantly faster than observed changes over the last 10,000 years, and would result in temperatures higher than those during the medieval warm period and the Holocene period of 6000 years ago. Associated with these estimated changes in temperature, sea level is projected to increase by 15 95 cm by 2100, caused primarily by thermal expansion of the oceans and the melting of glaciers.

Model calculations show that evaporation will be enhanced as the climate warms, and that there will be an increase in global mean precipitation and an increase in the frequency of intense rainfall. However, not all land regions will experience an increase in precipitation, and even those land regions with increased precipitation may experience decreases in soil moisture, because of enhanced evaporation. Seasonal shifts in precipitation are also projected. In general, precipitation is projected to increase at middle to high latitudes in winter, and soil moisture is projected to decrease in some mid-latitude continental regions during summer.

The incidence of extreme temperature events, floods, droughts, fires and pest outbreaks is expected to increase in some regions, but it is unclear whether there will be changes in the frequency and intensity of extreme weather events such as tropical storms, cyclones, and tornadoes.

While the reliability of regional scale predictions is still low, this does not preclude an assessment of the sensitivity of human health, ecological systems and socio-economic sectors to changes in climate. IPCC Working Group II primarily focused on evaluating the sensitivity and vulnerability of these systems to climate variability and changes in climate, e.g., it assessed how agricultural productivity would change as a result of an increase in temperature or a change in rainfall. This approach isolates the uncertainty in impacts analysis from uncertainties in regional projections of future climate. The lead authors reviewed and synthesized conclusions in the literature regarding thresholds and sensitivities of their systems to changes in climate variables. The response of a system to observed variability or an assumed change is determined through examination of laboratory and in situ studies. The assessment also examined the sensitivity of systems with respect to changes in climatic extremes, the effects of multiple environmental and anthropogenic stresses, the effects of different rates of change, and effects of other factors that would affect

Part II:

Human Health, Ecological systems, and Socio-economic Sectors are
all Vulnerable to Climate Change

IPCC Working Group II concluded that human-induced climate change is an important new stress, particularly on ecological and socio-economic systems that are already affected by pollution, increasing resource demands, and non-sustainable management practices. They noted that most systems are sensitive to both the magnitude and rate of climate change, but many of the impacts are difficult to quantify because existing studies are limited in scope. They also noted that successful adaptation depends upon technological advances, institutional arrangements, availability of financing and information exchange, and that vulnerability increases as adaptation capacity decreases.

Let me now briefly discuss the implications of climate change for a representative number of systems, i.e., human health, food security, natural ecosystems, and human habitats.

Human Health

Climate change is likely to have wide-ranging and mostly adverse impacts on human health, with significant loss of life. These impacts would arise by both direct and indirect pathways. Direct health effects include increases in (predominantly cardiorespiratory) mortality and illness due to an anticipated increase in the intensity and duration of heat waves. Indirect effects of climate change include increases in the potential transmission of vector-borne infectious diseases (e.g., malaria, dengue, yellow fever, and some viral encephalitis) resulting from extensions of the geographical range and season for vector organisms. This could lead to potential increases in malaria incidence of the order of 50-80 million additional annual cases, primarily in tropical, subtropical, and less well-protected temperate-zone populations. Some increases in non-vector-borne infectious diseases such as salmonellosis, cholera, and giardiasis-also could occur as a result of elevated temperatures and increased flooding.

Food Security

Existing studies show that on the whole, global agricultural production could be maintained relative to baseline production in the face of climate change under doubled equivalent CO2 equilibrium conditions. However, crop yields and changes in productivity due to climate change will vary considerably across regions and among localities, thus changing the patterns of production. Productivity is projected to increase in some areas and decrease in others, especially the tropics and subtropics. Therefore, there may be increased risk of hunger and famine in some locations in the tropics and subtropics where many of the world's poorest people live.

Natural Ecosystems

The composition and geographic distribution of many ecosystems will shift as individual species respond to changes in climate, and there will likely be reductions in biological diversity, and in the goods and services ecosystems provide society, e.g., sources of food, fibre, medicines, recreation and tourism, and ecological services such as controlling nutrient cycling, waste quality, water runoff, and soil erosion. Models project that as a consequence of possible changes in temperature and water availability under doubled equivalent-carbon dioxide equilibrium conditions, a substantial fraction (a global average of one-third, varying by region from one-seventh to two-thirds) of the existing forested area of the world will undergo major changes in broad vegetation types. Climate change is expected to occur at a rapid rate relative to the speed at which forest species grow, reproduce and re-establish themselves. Therefore, species composition of impacted forests is likely to change, and entire forest types may disappear while new assemblages of species and hence new forest ecosystems may be established. Coral reefs are the most biologically diverse marine ecosystems. Sustained increases in water temperatures of 3-4 °C above seasonal high average temperatures can cause significant coral mortality; short-term increases on the order of only 1-2 °C can cause "bleaching", leading to reef destruction.

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Human Habitat

Sea-level rise will increase the vulnerability of coastal populations to flooding. Model estimates put about 46 million people per year currently at risk of flooding due to storm surges; a 50 cm sea-level rise would increase this number to about 92 million; a 1 meter sea-level rise would increase this number to 118 million. The estimates will be substantially higher if one incorporates population growth projections. A number of studies have shown that small islands and delta areas are particularly vulnerable to a one-meter sea-level rise. Land losses ranged from 0.05% in Uruguay, 1.0% for Egypt, 6% for Netherlands, 17.5% for Bangladesh, to about 80% of the Marshall Islands, displacing tens of millions of people.

PART III:

Technical Options Exist to Reduce Emissions and Enhance Sinks of
Greenhouse Gases

Significant reductions in greenhouse gas emissions are technically possible and can be economically feasible. These reductions can be achieved by utilizing an extensive array of technologies and policy measures that accelerate technology development, diffusion, and transfer in all sectors, including the energy, industry, transportation, residential/commercial, and agricultural/forestry sectors.

Energy Demand

Numerous studies have indicated that it is possible to reduce energy demand: that 10-30% energy efficiency gains above present levels are feasible at little or no net cost in many parts of the world through technical conservation measures and improved management practices over the next 2 to 3 decades. Using technologies that presently yield the highest output of energy services for a given input of energy, efficiency gains of 50-60% would be technically feasible in many countries over the same time period. Achieving these potentials will depend on future cost reductions, financing and technology transfer, as well as measures to overcome a variety of non-technical barriers.

Energy Supply

It is technically possible to realize deep emissions reductions in the energy supply sector in step with the normal timing of investments to replace infrastructure and equipment as it wears out or becomes obsolete. Promising approaches, not ordered according to priority, include: more-efficient conversion of fossil fuels; switching to low-carbon fossil fuels and suppressing emissions; decarbonization of flue gases and fuels and carbon dioxide storage; switching to non-fossil fuel sources of energy such as nuclear energy or renewable fuels. Technological advances offer new opportunities and declining costs for energy from these sources.

Agriculture and Forestry

Beyond the use of biomass fuels to displace fossil fuels, the management of forests, agricultural lands, and rangelands can play an important role in reducing current emissions of carbon dioxide, methane, and nitrous oxide and enhancing carbon sinks. A number of measures could conserve and sequester substantial amounts of carbon (approximately an additional 60-90 GtC in the forestry sector alone) over the next 50 years. In the forestry sector, costs for conserving and sequestering carbon in biomass and soil are estimated to range widely but can be competitive with other mitigation options.

Policy Instruments

Policies are available to governments that facilitate the penetration of less greenhouse gas-intensive technologies and modified consumption patterns. Many countries have extensive experience with a variety of policies that can accelerate the adoption of such technologies. This experience comes from efforts over the past 20 to 30 years to achieve improved energy efficiency, reduce the environmental impacts of agricultural policies, and meet conservation and environmental goals unrelated to climate change. Policies to reduce net greenhouse gas emissions appear more easily

implemented when they are designed to address other environmental concerns (e.g. air pollution, and soil erosion). These policies include: (i) voluntary programs and negotiated agreements with industry; (ii) utility demand-side management programs; (iii) tradable emissions permits; (iv) energy pricing strategies-for example, carbon or energy taxes, and reduced energy subsidies; (v) renewable energy incentives during market build-up; (vi) incentives such as provisions for accelerated depreciation and reduced costs for consumers; (vii) reducing or removing other subsidies, for example agricultural and transport subsidies, which increase greenhouse gas emissions; (viii) regulatory programs including minimum energy-efficiency standards, such as for appliances and fuel economy; (ix) stimulating research, development, and demonstration to make new technologies available.

PART IV: Conclusion

Policymakers are faced with responding to the risks posed by anthropogenic emissions of greenhouse gases in the face of significant scientific uncertainties. They should note though, that uncertainties go in two directions, i.e., the models may be either over-estimating or underestimating the impact of human activities on the Earth's climate. In addition, policymakers should consider these uncertainties in the context of information indicating that climate-induced environmental changes cannot be reversed quickly, if at all, due to the long time scales (decades to millennia) associated with the climate system. Decisions taken during the next few years may limit the range of possible policy options in the future because high near-term emissions would require deeper reductions in the future to meet any given target concentration. Delaying action might reduce the overall costs of mitigation because of potential technological advances but could increase both the rate and the eventual magnitude of climate change, and hence the adaptation and damage costs. Policymakers will have to decide to what degree they want to take precautionary measures by mitigating greenhouse gas emissions and enhancing the resilience of vulnerable systems by means of adaptation. Uncertainty does not mean that a nation or the world community cannot position itself better to cope with the broad range of possible climate changes or protect against potentially costly future outcomes. Delaying such measures may leave a nation or the world poorly prepared to deal with adverse changes and may increase the possibility of irreversible or very costly consequences.

While human-induced climate change is a serious environmental issue, it is also clear that improved scientific knowledge and technological advances, coupled with strong policy measures, can allow society to significantly reduce greenhouse gas emissions in a cost-effective manner. However, to achieve this goal will require that a priority be placed on research and development in a number of areas: (i) an improved understanding of how human activities change climate at the regional scale; (ii) an improved understanding of how human health, ecological and socio-economic systems respond to changes in climate; (iii) the development of cost-effective adaptation strategies; and (iv) the development of improved energy efficiency technologies and low greenhouse gas emission energy supply technologies. A coordinated effort to address the climate change issue by the scientific community, industry, business, environmental organizations and governments, all working towards the common goal of the cost-effective protection of human health and our vital economic and ecological systems, is within our grasp.

Annex I

Background Information

on the

Intergovernmental Panel on Climate Change

The Intergovernmental Panel on Climate Change (IPCC) was established in 1988 by the United Nations Environment Programme (UNEP) and the World Meteorological Organization (WMO). Its purpose is to assess scientific and technical information about climate change.

Previous Reports

In the 7 years since its inception, the IPCC has prepared a series of reports and methodologies, including:

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The 1990 comprehensive three-volume assessment of climate change, which evaluated anthropogenic alteration of the climate system, potential impacts, and available response measures (IPCC, 1990). This report became a standard reference, widely used by policymakers, scientists, and other experts.

A supplementary review of literature related to climate change, impacts, and response measures prepared for the U.N. Conference on Environment and Development (UNCED) (IPCC, 1992).

A special report on radiative forcing of climate and greenhouse gas emissions scenarios, produced for the first meeting of the Conference of Parties to the U.N. Framework Convention on Climate Change (UNFCCC) (IPCC, 1994a).

The IPCC methodology for assessing climate change impacts and adaptation measures (IPCC, 1994b).

The IPCC, Organisation for Economic Cooperation and Development (OECD), and International Energy Agency (IEA) methodology for conducting and reporting on national inventories of greenhouse gas emissions (IPCC, 1995).

These publications have established a common body of scientific information that has been used by governments in international negotiations and national decisionmaking.

New Reports

At the request of governments, the IPCC is currently preparing its Second Assessment Report (SAR), which will provide a comprehensive assessment of new and recent literature. To be completed at the end of 1995, the SAR will be published in three volumes, plus a special report. The common title for all of the volumes is Climate Change 1995: The IPCC Second Assessment Report. Titles of the separate volumes (to be contributed by Working Groups I through III) and the special report follow:

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Volume 2: Scientific-Technical Analyses of Impacts, Adaptations, and Mitigation of
Climate Change

Volume 3: Economics and Social Dimensions

The IPCC Synthesis Report: An Assessment of Scientific-Technical Information Relevant to Interpreting Article 2 of the U.N. Framework Convention on Climate Change, and the

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