At an Intergovernmental Panel on Climate Change (IPCC) conference in April 2007, delegates from 120 nations discussed the specific economic and societal costs of mitigating global warming, and eventually approved the IPCC Fourth Assessment Report.
Projections of climate change
Integrated assessment models provide different projections as to the amount of future climate change. The IPCC have produced a report (SRES) where a number of different future scenarios are described. The scenarios differ in whether the future will be:
* 'more environmental' (scenarios with the 'B' prefix) or 'market-oriented' (scenarios with the 'A' prefix)
* 'more global' (scenarios with the '1' suffix) or 'more regional' (scenarios with the '2' suffix)
Forecasts of changes in global mean temperature for these scenarios are given in the IPCC report.The 'best estimate' global mean temperature increase (2090 to 2099 relative to the period 1980-1999) for these scenarios range from 1.8 degrees Celsius for the B1 scenario, to 4.0 degrees Celsius for the A1FI scenario. The 'likely' range (greater than 66% probability) over the same period for all the SRES scenarios is a global mean temperature increase of between 1.1 to 6.4 degrees Celsius.
A 2009 study by the MIT Joint Program on the Science and Policy of Global Change looked at future predictions of climate change.According to this study, there is a 57% likelihood of exceeding a 5 degrees Celsius increase in global mean temperature by 2100 (relative to the base years of 1981 to 2000). This is the 'no policy' estimate. In the 'policy' estimate, where greenhouse gas emissions are controlled to relatively low levels, the likeliest increase in global mean temperature for the same period is between 2 and 2.5 degrees Celsius.
According to a 2008 study by the Hadley Centre, for a 'business-as-usual' increase in global greenhouse gas emissions of 132% (from 1990 emission levels) by 2050, the rise in global mean temperature will be between 5.5 and 7.1 degrees Celsius (relative to pre-industrial levels) by 2100.In this estimate, the likeliest increase in global mean temperature is 5.5 degrees Celsius (50% chance of occurring), and the the worst case increase in global mean temperature is 7.1 degrees Celsius (10% chance of occurring). The Hadley Centre study also looked at other emissions scenarios. In a scenario where there is an early and rapid decline in emissions (a 47% decrease from 1990 emission levels by 2050), global mean temperature is predicted to rise 2.1 to 2.8 degrees Celsius by 2100. For this scenario, 2.1 degrees Celsius is the likeliest increase in global mean temperature (50% chance of occurring), and 2.8 degrees Celsius the worst case increase in global mean temperature (10% chance of occurring).
Economic impacts of global warming
Aggregate impacts
The IPCC Fourth Assessment Report, published in 2007, looked at the aggregate economic impacts of climate change:
to impose net annual costs, which will increase over time as global temperatures increase. Peer-reviewed estimates of the social cost of carbon in 2005 average US$12 per tonne of CO2, but the range from 100 estimates is large (-$3 to $95/tCO2). This is due in large part to differences in assumptions regarding climate sensitivity, response lags, the treatment of risk and equity, economic and non-economic impacts, the inclusion of potentially catastrophic losses and discount rates. Aggregate estimates of costs mask significant differences in impacts across sectors, regions and populations and very likely underestimate damage costs because they cannot include many non-quantifiable impacts.
Aggregate impacts have also been quantified in other metrics: for example, climate change over the next century is likely to adversely affect hundreds of millions of people through increased coastal flooding, reductions in water supplies, increased malnutrition and increased health impacts.
According to the IPCC Report, with medium confidence (around 5/10 chance of being correct): 'aggregate market sector impacts of 2°C global mean temperature increase, above the 1990 level, will be plus or minus a few percent of global GDP, with most people in the world negatively affected. Studies of aggregate economic impacts found net damages beyond temperature increases of 2 to 3°C above 1990 levels, with increasing damages at higher magnitudes of climate change.' The Report adds that: 'On balance, the current generation of aggregate estimates in the literature is more likely than not to understate the actual costs of climate change.'
The Copenhagen Consensus
As part of the 2004 Copenhagen Consensus on the economics of global warming, Professor Robert O. Mendelsohn of Yale School of Forestry and Environmental Studies, stated that:
A series of studies on the impacts of climate change have systematically shown that the older literature overestimated climate damages by failing to allow for adaptation and for climate benefits (see Fankhauser et al. 1997; Mendelsohn and Newmann 1999; Tol 1999; Mendelsohn et al. 2000; Mendelsohn 2001;Maddison 2001; Tol 2002; Sohngen et al. 2002; Pearce 2003; Mendelsohn and Williams 2004). These new studies imply that impacts depend heavily upon initial temperatures (latitude). Countries in the polar region are likely to receive large benefits from warming, countries in the mid-latitudes will at first benefit and only begin to be harmed if temperatures rise above 2.5C (Mendelsohn et al. 2000). Only countries in the tropical and subtropical regions are likely to be harmed immediately by warming and be subject to the magnitudes of impacts first thought likely (Mendelsohn et al. 2000). Summing these regional impacts across the globe implies that warming benefits and damages will likely offset each other until warming passes 2.5C and even then it will be far smaller on net than originally thought (Mendelsohn and Williams 2004)."
The Stern Review
The Stern Review is a 2006 reportby the former Chief Economist and Senior Vice-President of the World Bank, Nicholas Stern, which predicts that climate change will have a serious impact on economic growth without mitigation.The report suggests that an investment of one percent of global GDP is required to mitigate the effects of climate change, with failure to do so risking a recession worth up to twenty percent of global GDP.
In the Stern Review, net monetised cost estimates of climate change were negative (i.e., net damages) for all global mean temperature increases. The Review has been criticized by some economists, saying that Stern did not consider costs past 2200, that he used an incorrect discount rate in his calculations, and that stopping or significantly slowing climate change will require deep emission cuts everywhere.
Some economists have supported Stern's approach, or argued that Stern's estimates are reasonable, even if the method by which he reached them is open to criticism. Research by Weitzman has suggested that structural uncertainty and low-probability high-impact risks are very important, and that "the influence on cost-benefit analysis of fat-tailed structural uncertainty about climate change, coupled with great unsureness about high-temperature damages, can outweigh the influence of discounting or anything else".
Criticism of aggregate costs
Some experts are critical of how economic studies aggregate costs of climate change damage.Schneider and Lane argue that because of the problems of one-metric aggregations, multiple metrics should be used to assess climate change damages.
Monetising aggregate costs of climate change often requires valuations of human welfare, the state of the environment, etc. This process is called using surrogate prices. The methodology and results of calculating surrogate prices has been described as 'problematical' by Ackerman.Using the example of the First and Second World Wars, Jaeger et al. argue that human suffering is 'incommensurable with GDP figures'.
Schneider and Lane point to the inadequacies of market-aggregation-only analysis, using Bangladesh as an example. Sea level rise due to climate change could reduce Bangladesh's GDP by about 80%, but this would only be equivalent to a reduction in global GDP of 0.1%. In a market-aggregation-only analysis, a loss of 0.1% global GDP would be described as being relatively insignificant. Schneider and Lane dispute this result, arguing that loss of life and biodiversity in Bangladesh are 'at least as important as aggregate market impacts'.
Distribution of impacts
According to the IPCC report: 'here is medium confidence that a warming of less than 2°C above 1990 levels would have net negative impacts on market sectors in many developing countries and net positive impacts on market sectors in many developed countries; and high confidence that above 2 to 3°C, there would be net negative impacts in many developed countries and additional negative impacts in many developing countries.'
Vulnerability to climate change is highly variable within individual countries. As a consequence, some population groups in developed countries are also highly vulnerable to a warming of less than 2°C.
Water
All IPCC regions show an overall net negative impact of climate change on water resources and freshwater ecosystems. Efforts to quantify the economic impacts of climate-related changes in water resources are hampered by a lack of data. Additionally, cost estimates are highly sensitive to different estimation methods and to different assumptions regarding how changes in water availability will be allocated across various types of water uses, e.g., between agricultural, urban, or in-stream uses.
Effects on agriculture
In the Summary for Policy Makers of the 4th Assessment Report, Working Group II of the Intergovernmental Panel on Climate Change states that: "Crop productivity is projected to increase slightly at mid- to high latitudes for local mean temperature increases of up to 1-3°C depending on the crop, and then decrease beyond that in some regions. At lower latitudes, especially seasonally dry and tropical regions, crop productivity is projected to decrease for even small local temperature increases (1-2°C), which would increase the risk of hunger. Globally, the potential for food production is projected to increase with increases in local average temperature over a range of 1-3°C, but above this it is projected to decrease."
Insurance
An industry very directly affected by the risks is the insurance industry; the number of major natural disasters has tripled since the 1960s, and insured losses increased fifteenfold in real terms (adjusted for inflation). According to one study, 35–40% of the worst catastrophes have been climate change related (ERM, 2002). Over the past three decades, the proportion of the global population affected by weather-related disasters has doubled in linear trend, rising from roughly 2% in 1975 to 4% in 2001 (ERM, 2002).
According to a 2005 report from the Association of British Insurers, limiting carbon emissions could avoid 80% of the projected additional annual cost of tropical cyclones by the 2080s. A June 2004 report by the Association of British Insurers declared "Climate change is not a remote issue for future generations to deal with. It is, in various forms, here already, impacting on insurers' businesses now." It noted that weather risks for households and property were already increasing by 2-4 % per year due to changing weather, and that claims for storm and flood damages in the UK had doubled to over £6 billion over the period 1998–2003, compared to the previous five years. The results are rising insurance premiums, and the risk that in some areas flood insurance will become unaffordable for some.
Financial institutions, including the world's two largest insurance companies, Munich Re and Swiss Re, warned in a 2002 study that "the increasing frequency of severe climatic events, coupled with social trends" could cost almost US$150 billion each year in the next decade.These costs would, through increased costs related to insurance and disaster relief, burden customers, taxpayers, and industry alike.
In the United States, insurance losses have also greatly increased. According to Choi and Fisher (2003) each 1% increase in annual precipitation could enlarge catastrophe loss by as much as 2.8%. Gross increases are mostly attributed to increased population and property values in vulnerable coastal areas, though there was also an increase in frequency of weather-related events like heavy rainfalls since the 1950s
Infrastructure
Roads, airport runways, railway lines and pipelines, (including oil pipelines, sewers, water mains etc) may require increased maintenance and renewal as they become subject to greater temperature variation and are exposed to weather that they were not designed for. Regions already adversely affected include areas of permafrost, which are subject to high levels of subsidence, resulting in buckling roads, sunken foundations, and severely cracked runways.
Investment
Venture capitalists and other investors have noted potential opportunities arising from global warming, as massive sums of money are needed for enhanced infrastructure as well as clean technologies that could help reduce emissions of global warming gases. As Joel Makower, a noted expert on business and the environment, has pointed out, "For all the handwringing over the negative bottom-line impacts of climate change for most companies, a handful of large corporate interests may come out winners, creating potentially profitable opportunities for forward-thinking investors." These include companies investing in clean energy technologies such as solar energy and wind power, but also companies in other sectors: agriculture (to produce biofuels as well as biobased plastics that supplant petroleum-based ones), information technology companies (producing switches, routers, and software intended to create a more efficient, "smart grid", chemical companies (producing "green chemistry" alternatives to petrochemicals), and producers of more efficient motors for aircraft, automobiles, and industrial use.
Migration
Some Pacific Ocean island nations, such as Tuvalu, are concerned about the possibility of an eventual evacuation, as flood defense may become economically inviable for them. Tuvalu already has an ad hoc agreement with New Zealand to allow phased relocation.
In the 1990s, a variety of estimates placed the number of environmental refugees at around 25 million. (Environmental refugees are not included in the official definition of refugees, which only includes migrants fleeing persecution.) The Intergovernmental Panel on Climate Change (IPCC), which advises the world’s governments under the auspices of the UN, estimated that 150 million environmental refugees will exist in the year 2050, due mainly to the effects of coastal flooding, shoreline erosion and agricultural disruption (150 million means 1.5% of 2050’s predicted 10 billion world population).
Northwest Passage
Melting Arctic ice may open the Northwest Passage in summer, which would cut 5,000 nautical miles (9,000 km) from shipping routes between Europe and Asia. This would be of particular relevance for supertankers which are too big to fit through the Panama Canal and currently have to go around the tip of South America. According to the Canadian Ice Service, the amount of ice in Canada's eastern Arctic Archipelago decreased by 15% between 1969 and 2004.
While the reduction of summer ice in the Arctic may be a boon to shipping, this same phenomenon threatens the Arctic ecosystem, most notably polar bears which depend on ice floes. Subsistence hunters such as the Inuit peoples will find their livelihoods and cultures increasingly threatened as the ecosystem changes due to global warming.
Development
The combined effects of global warming may impact particularly harshly on people and countries without the resources to mitigate those effects. This may slow economic development and poverty reduction, and make it harder to achieve the Millennium Development Goals.
In October 2004, the Working Group on Climate Change and Development, a coalition of development and environment NGOs, issued a report Up in Smoke on the effects of climate change on development. This report, and the July 2005 report Africa - Up in Smoke? predicted increased hunger and disease due to decreased rainfall and severe weather events, particularly in Africa. These are likely to have severe impacts on development for those affected.
At the same time, in developing countries, the poorest often live on flood plains, because it is the only available space, or fertile agricultural land. These settlements often lack infrastructure such as dykes and early warning systems. Poorer communities also tend to lack the insurance, savings or access to credit needed to recover from disasters.
Environmental
Assessing the economic value of ecosystems and biodiversity is difficult,but attempts have been made to do this. Stern presents the results of several integrated assessment models that include climate change impacts on ecosystems.
Non-monetised impacts of climate change on ecosystems and biodiversity are assessed in the IPCC report:of the species assessed so far, there is medium confidence (around 5/10 chance of being correct) that 20-30% will be at increased risk of extinction if global mean temperature increase exceeds 1.5-2.5 degrees Celsius (relative to the period 1980-1999). This temperature increase would be expected to have a predominantly negative impact on biodiversity and ecosystem goods and services, e.g. water and food supply.
Smith and Hitz looked at climate change impacts on terrestrial ecosystems.According to the paper, increased atmospheric concentrations of carbon dioxide - associated with the burning of fossil fuels - will be of some benefit to plant growth. Vegetation productivity is expected to peak then decline with increasing global mean temperature.
A 2004 study published in Nature estimates that between 15 and 37% of known plant and animal species will be 'committed to extinction' by 2050. Few of the terrestrial ecoregions on Earth could expect to be unaffected.
Water scarcity
Positive eustasy (sea-level rise) may contaminate groundwater, affecting drinking water and agriculture in coastal zones. Increased evaporation will reduce the effectiveness of reservoirs. Increased extreme weather means more water falls on hardened ground unable to absorb it, leading to flash floods instead of a replenishment of soil moisture or groundwater levels. In some areas, shrinking glaciers threaten the water supply. The availability of freshwater runoff from mountains for natural systems and human uses may also be impacted.
Higher temperatures will also increase the demand for water for the purposes of cooling and hydration.
Health
Currently, climate change contributes to increased early deaths and the burden of disease[. Climate change is expected to have a predominantly negative effect on human health, particularly in low-income countries . An example of a health benefit of climate change is fewer cold deaths. Some examples of negative health effects include:
* increased levels of malnutrition
* increased deaths, diseases, and injuries due to extreme weather events
* greater burden of diarrhoeal diseases
Some economists have included health outcomes in cost-benefit studies of climate change. These studies have several shortcomings; one is that they only cover a limited range of health outcomes, e.g., malaria, heat and cold deaths. In these studies, as is traditional in economics, the value of human mortality in poorer countries is judged to be lower than human mortality in richer countries. One study has suggested that replacing national mortality values with a global average would increase mortality costs by up to five times.
Heat and cold health effects
In temperate areas, warming of the climate is expected to bring some benefits, such as reduced numbers of deaths due to cold exposure. This benefit is expected to be outweighed by the negative effects of temperature rise, especially in developing countries.
Palutikof et al. calculate that in England and Wales for a 1 °C temperature rise the reduced deaths from cold outweigh the increased deaths from heat, resulting in a reduction in annual average mortality of 7000. However, in the United States, only 1000 people die from the cold each year, while twice that number die from the heat. The 2006 United States heat wave killed at least 225 people, with 163 of those in California. The central California valley, had six consecutive days of 110 degree-plus Fahrenheit temperatures.
The European heat wave of 2003 killed 22,000–35,000 people, based on normal mortality rates (Schär and Jendritzky, 2004). It can be said with 90% confidence that past human influence on climate was responsible for at least half the risk of the 2003 European summer heat-wave (Stott et al. 2004).
Spread of disease
Global warming is expected to extend the favourable zones for vectors conveying infectious disease such as malaria. In poorer countries, this may simply lead to higher incidence of such diseases. In richer countries, where such diseases have been eliminated or kept in check by vaccination, draining swamps and using pesticides, the consequences may be felt more in economic than health terms, if greater spending on preventative measures is required.
Contamination by sector and cost of reducing fossil fuel use
Reducing greenhouse gas emissions depends in part on lowering consumption of fossil fuels. The key challenge is that nearly all forms of economic activity rely on fossil fuel energy sources, from transportation fuel, electricity from coal-fired plants, industrial furnaces to home and office heating. Reducing emissions can be achieved through gains in efficiency - producing the same benefits with smaller amounts of fossil energy, or by displacing fossil sources with non- or low-emitting sources. Low emission renewable energy sources such as wind, solar and biomass still represent only a small fraction of total energy consumption. The scale of current fossil energy dependence poses a substantial challenge. Gaining energy efficiency typically requires up-front investment, such as adding insulation, replacing energy-inefficient devices and processes, or buying hybrid vehicles. Some such investments can pay for themselves in the savings on energy bills, and the economic case for choosing them depends on the payback period. If an upgrade's payback is better than the risk-free interest rate, economic theory predicts individuals will choose the higher return of making the efficiency investment. If current pricing is not leading to this outcome, the cost of fossil energy is not yet high enough to drive adoption of available efficiency gains. (Social science researchers Kurani and Turrentine reported in 2004 that consumers often fail to make choices that have favorable payback period. They attribute the "uneconomic" choices to risk aversion, weighing potential losses much higher than potential gains.)
Advocates of mitigating climate change hold that greenhouse gas emissions must carry a price, so the market can internalize the externality of the impact of their emission. This could take the form of a carbon tax or of emission caps, with a market created for trading emission permits, much as was done in the USA for sulfate emissions blamed for acid rain. Thus the economic impact of avoiding greenhouse gas emissions depends on how much consumption will have to be avoided, and how quickly the economy can incorporate efficiency gains.
Some pundits have criticized such attempts at calculating the costs of mitigating climate change by avoiding fossil fuel consumption, pointing out that the opportunity costs of avoiding consumption are not (and cannot) be calculated and are likely to be more important than the expected benefits .
Mitigation and adaptation
The costs of mitigating (reducing) global warming depend on a number of factors. One fundamental factor is the target level of atmospheric carbon dioxide: the lower the level, the sooner action must be taken if increases beyond the target level are to be avoided. The sooner action must be taken, the shorter the period over which costs must be spread, and the higher the absolute costs, as cheaper technologies which might emerge later are not yet available. A common target level (assumed by the United Kingdom) is 550ppm (current levels are around 380ppm, and rising at 2-3ppm per year). Signatories of the Kyoto Protocol committed themselves to targets that require lowering their national greenhouse gas emissions to a specified level relative to their actual 1990 emissions. During the target period for Kyoto of 2008-2012, many nations set targets to reach a small percentage below 1990 levels.
Another crucial factor in estimating the costs of climate change is the discount rate to apply. Normally a relatively high rate (e.g. 5%-10%) is applied, reflecting the cost of capital. However, where intergenerational issues involve potential irreversibilities such as climate change, a low discount rate (e.g. 1%-4%) may be applied. The difference is dramatic: at 4% (a typical rate for social issues), avoiding $1m worth of climate change damage in 100 years' time is valued at nearly $20,000 today (net present value), whereas at 8% it is valued at less than $500.
Another area for debate is the relationship between technological development and regulatory incentives: if regulation can induce substantial technological change, the costs of mitigation may be much lower.
The Kyoto Protocol
According to the IPCC report, 'notable achievements' of the UNFCCC and the Kyoto Protocol include:
* the establishment of a global response to the climate problem;
* the stimulation of an array of national policies;
* the creation of an international carbon market;
* the establishment of new institutional mechanisms that may provide the foundation for future mitigation efforts.
Significant differences exist between countries in meeting their Kyoto commitments. Collectively, industrial countries who ratified the treaty will probably meet their 2010 emission limitation targets.
The Kyoto Protocol was the first international agreement to set mandatory limits on greenhouse gas emissions. Kyoto's emission reduction targets have been criticised, with some saying they are too weak and others saying they are too strong. The IPCC report describes Kyoto's emission reduction targets as being 'modest', and to be more effective, 'future mitigation efforts would need to achieve deeper reductions covering a higher share of global emissions'.
Tol has stated that "the emissions targets agreed in the Kyoto Protocol are irreconcilable with economic rationality." Nordhaus and Boyer estimated that the present value of benefits from mitigation under the Kyoto Protocol would be $120 billion, far below the likely costs; "Other studies reach similar conclusions". Grubb has criticised cost-benefit analyses of this sort, arguing that they suffer from a number of problems.
Some economists view Kyoto as a useful first step in responding to climate change. Climate scientists O'Neill and Oppenheimer support Kyoto's targets, arguing that they are consistent with atmospheric CO2 stabilization at 450 ppm. A 450 ppm target could 'forestall the disintegration of WAIS, but is by no means certain, because additional warming would occur beyond 2100'.
Cost estimates
IPCC TAR (Synthesis Report) suggested values of $78 billion to $1141 billion annual mitigation costs, amounting to 0.2% to 3.5% of current world GDP (which is around $35 trillion), or 0.3% to 4.5% of GDP if borne by the richest nations alone. As economic growth is expected to continue, the percentage would fall. In terms of cost per tonne of carbon emission avoided, the range (for a target of 550ppm) is $18 to $80.
These cost estimates refer to reductions achieved through tradable emissions permits when those permits are given away to polluters. If the reductions are achieved through emission taxes or auctioned permits, and the revenue is used to reduce distortionary taxes, the TAR III synthesis report concludes that " on the existing tax structure, type of tax cuts, labour market conditions and method of recycling... it is possible that the economic benefits may exceed the costs of mitigation." Nordhaus and Boyer calculated that the present value cost of the Kyoto Protocol would be $800 billion to $1,500 billion if implemented as efficiently as possible. Richard Tol estimates that the net present value cost to be more than $2.5 trillion.
Azar and Schneider (2002) observe that global output in 1990 was around $20 trillion. If it grew steadily at 2.1 percent per annum it would be just short of $200 trillion by 2100. They thereby make the point that the calculated present value costs of mitigation would look smaller if scaled against 2100 output than if scaled against 1990 output. However, neither comparator is relevant to the question of whether the likely benefits from mitigation exceed the costs.
A 2008 study, not peer-reviewed, by the consulting company McKinsey Global Institute uses cost curve analysis to estimate that it is possible to stabilize global greenhouse gas concentrations at 450 to 500 ppm CO2-e with macroeconomic costs in the order of 0.6-1.4% of global GDP by 2030.
Lord Peter Levene, chairman of Lloyd's of London, said on 12 April 2007 that the threat of climate change must be an integral part of every company’s risk analysis.
Co-benefits
In addition to avoiding the costs of the business-as-usual scenario, mitigation actions can bring other benefits, depending on factors such as the technology used. These include, for example, the reduced economic impact from oil supply disruptions and/or price rises, if mitigation reduces oil dependence. This may be of particular benefit to non-oil-exporting developing countries, which suffer greater economic impact from oil price rises. Co-benefits from ending deforestation include protection of biodiversity, benefits for indigenous people, research and development possibilities, tourism, and some protection from extreme weather events. (Stern Review, page 280) Reducing greenhouse gas emissions also significantly reduces air pollution.
Optimal strategies for mitigation
Financial and technological strategies can have a major impact on reaching a particular target atmospheric greenhouse gas concentration.
* Carbon tax
* Carbon emissions trading
* A hybrid between a carbon tax and an emissions trading scheme, this can be thought of as an emissions trading scheme with a price cap, a price floor, or both. A price cap can be realized by governments being able to sell an unlimited amount extra permits at a given price (the price of the cap). A price floor can be realized by governments buying back permits if the price goes below the value of the floor, or by emitters paying a fee when they exercise the permit (so the effective carbon price is equal to the sum of the permit price and the exercise fee).
* Regulation
* Reducing the carbon intensity of energy via Nuclear power or Renewable Energy
* Energy efficiency
"No regrets" policies - notably reducing fossil fuel subsidies, which is predicted to increase growth whilst reducing CO2 emissions. Article 2 of the Kyoto Protocol specifies a progressive removal of subsidies and reform of taxes as a means of achieving reduction commitments.
McKibbin and Wilcoxen argue that a combination of long term carbon price signals and short terms caps on economic cost is needed to address both economic efficiency, equity sharing and political feasibility.
The Stern Review recommends adopting a quantative global stabilisation target range for the stock of greenhouse gases as a foundation for policy. It suggests that this target range would be likely to be somewhere between 450-550 ppm CO2-e. It also recommends a carbon price signal through the use of a carbon tax or emissions trading scheme.
Brink et al. (2005) showed that the costs of mitigation can be reduced by considering the inter-relationships of different greenhouse gas, and the differential impact that different technological decisions may have on their emissions.
Cost distribution
The costs and benefits of global warming are distributed quite unequally.
* low-lying countries' risk of floods
* many countries subject to increased drought are poor African countries
* ability of poor countries to mitigate / adapt (margin)
* GW increases variability of weather, which implies greater capital requirements for water storage systems, flood defenses, etc as well as individual requirements to cope with wider variation in weather patterns
The costs of mitigation may also be distributed unequally, both within and between countries. Wier et al. (2005) showed that carbon taxes, particularly direct taxes on households, are regressive (more so than VAT), suggesting that in order to maintain social acceptance the regressive effect needs to be compensated for either within the environmental tax structure, or in other parts of the tax system. Indirect taxes (on business) are less regressive, and petrol taxes are found to be progressive.
Inter-relationships between countries
Bastianoni et al. (2004) note the differences between methodologies for assigning responsibility for greenhouse gas emissions, which include the geographical approach, based on the IPCC guidelines for GHG inventory; the consumer responsibility approach, based on the Ecological Footprint methodology; and the Carbon Emission Added (CEA) approach, which resembles the accounting of a Value Added Tax. Different methodologies can produce quite different results in terms of responsibility for emissions, with consequent impact on policy.
Gradual change vs climate surprises
Baranzini et al. (2003) conclude that "(i) gradual, continuous uncertainty in the global warming process is likely to delay the adoption of abatement policies as found in previous studies, with respect to the standard CBA; however (ii) the possibility of climate catastrophes accelerates the implementation of these policies as their net discounted benefits increase significantly."
From http://en.wikipedia.org/
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