There are only a few days left to submit a paper to IAEE 2013. It overlaps with IEW 2013 so you can't got to both. I would love to visit Korea again though and the IAEE meeting in Perth last year was pretty good. But even if my abstract isn't accepted at IEW, I still want to go to Europe so I think I'll drop the idea of going to Korea.
Signs of Fracking
For more around a decade methane concentrations in the atmosphere were pretty much constant from year to year. In the last few years they have begun to creep up again Is that the sign of the fracking boom? Some research finds that methane leakage from fracking is much greater than from traditional gas fields and supply networks. We estimated that gas supply was the smallest anthropogenic source and gas flaring had declined from its peak contribution:
Flaring might also be again increasing. Climate Progress posted this image of gas flaring in North Dakota:
Friday, January 4, 2013
World Scientific Output
From Information Processing - Number of scientific papers in 2012 and proportion of highly cited ones.
Australia (population = 23 million) has a decent showing with roughly double the output of Sweden (9.5 million) in terms of total papers and highly cited ones and half the output of the UK (63 million).
Australia (population = 23 million) has a decent showing with roughly double the output of Sweden (9.5 million) in terms of total papers and highly cited ones and half the output of the UK (63 million).
Thursday, January 3, 2013
Other Emissions of Greenhouse Gases and Aerosols
I only cover three other types of emissions besides energy related CO2. I thought of including black carbon but in the end decided to skip it as I already have too many papers. I resisted the temptation to try to include two of my papers in the collection, though I ended up discussing my paper more below :) I also include a graphic that will not be appearing in our book. It is from Smith et al. (2011) and compares the various estimates of sulfur emissions.
Deforestation and land-use change is an important source of emissions of CO2. Levels of emissions are much lower than from energy related sources, more stable over time, but also very uncertain. Houghton (2003) presents estimates of CO2 emissions from land-use change from 1850 to 2000, globally and by region. In general the tend rises from 1 to 2 Gt C over the 150 years with an acceleration in the trend around 1950 in common with emissions from energy related sources. Therefore, there is a clear link with economic growth. Tropical deforestation, particularly in Asia and Latin America dominates. In recent decades there is net reforestation in developed countries. Unusually, the data are increasingly uncertain in recent decades with estimates from different researchers varying substantially (Houghton, 2010).
The third most important greenhouse gas in the atmosphere and the second most important anthropogenic source is methane. Relatively little work has been done on CH4 in comparison to CO2. Stern and Kaufmann (1996) used available data to reconstruct the first time series of historic emissions from 1860-1993. They found that anthropogenic emissions had increased from 80 million tonnes of carbon in 1860 to 380 million in 1990. The relative importance of the various emissions sources changed over time though rice farming and livestock husbandry remained the two most important sources.
Offsetting the radiative forcing due to greenhouse gases is a significant negative forcing due to aerosols derived from sulphur oxide (primarily dioxide) emissions. These aerosols do not persist in the atmosphere for usually more than a few days and so the source of emissions is important and effects are localized though they spread far beyond the sources to affect neighbouring countries. The main sources of anthropogenic sulphur emissions are the combustion of coal and metal smelting. Stern (2006) showed that that after increasing fairly steadily from 1850 to the early 1990s global emissions began to trend downwards. Emissions in Western Europe and North America as well as Japan had already been trending down since 1970 primarily due to policies to reduce acid rain (Stern, 2005). But this decline was offset by growth in other regions. Following 1990, there was a dramatic reduction in emissions from Eastern Europe and the former Soviet Union. The likelihood that emissions will continue to decline in the future will contribute to future warming. Whereas Stern (2006) uses a combination of previously published data and model estimates, Smith et al. (2011) provide an inventory of sulphur emissions from 1850 to 2005 using a uniform methodology. The results largely confirm Stern’s (2006) findings though the levels are generally lower by a few percent.
References
Houghton, R. A. (2003) Revised estimates of the annual net flux of carbon to the atmosphere from changes in land use and land management 1850-2000, Tellus 55B: 378-390.
Houghton, R. A. (2010) How well do we know the flux of CO2 from land use change? Tellus 62B: 337-351.
Smith, S. J., J. van Ardenne, Z. Klimont, R. J. Andres, A. Volke, S. D. Arias (2011) Anthropogenic sulfur dioxide emissions: 1850-2005, Atmospheric Chemistry and Physics 11: 1101-1116.
Stern D. I. (2005) Beyond the environmental Kuznets curve: Diffusion of sulfur-emissions-abating technology, Journal of Environment and Development 14(1), 101-124.
Stern D. I. (2006) Reversal in the trend of global anthropogenic sulfur emissions, Global Environmental Change 16(2), 207-220.
Stern D. I. and R. K. Kaufmann (1996) Estimates of global anthropogenic methane emissions 1860-1993, Chemosphere 33, 159-176.
Deforestation and land-use change is an important source of emissions of CO2. Levels of emissions are much lower than from energy related sources, more stable over time, but also very uncertain. Houghton (2003) presents estimates of CO2 emissions from land-use change from 1850 to 2000, globally and by region. In general the tend rises from 1 to 2 Gt C over the 150 years with an acceleration in the trend around 1950 in common with emissions from energy related sources. Therefore, there is a clear link with economic growth. Tropical deforestation, particularly in Asia and Latin America dominates. In recent decades there is net reforestation in developed countries. Unusually, the data are increasingly uncertain in recent decades with estimates from different researchers varying substantially (Houghton, 2010).
The third most important greenhouse gas in the atmosphere and the second most important anthropogenic source is methane. Relatively little work has been done on CH4 in comparison to CO2. Stern and Kaufmann (1996) used available data to reconstruct the first time series of historic emissions from 1860-1993. They found that anthropogenic emissions had increased from 80 million tonnes of carbon in 1860 to 380 million in 1990. The relative importance of the various emissions sources changed over time though rice farming and livestock husbandry remained the two most important sources.
Offsetting the radiative forcing due to greenhouse gases is a significant negative forcing due to aerosols derived from sulphur oxide (primarily dioxide) emissions. These aerosols do not persist in the atmosphere for usually more than a few days and so the source of emissions is important and effects are localized though they spread far beyond the sources to affect neighbouring countries. The main sources of anthropogenic sulphur emissions are the combustion of coal and metal smelting. Stern (2006) showed that that after increasing fairly steadily from 1850 to the early 1990s global emissions began to trend downwards. Emissions in Western Europe and North America as well as Japan had already been trending down since 1970 primarily due to policies to reduce acid rain (Stern, 2005). But this decline was offset by growth in other regions. Following 1990, there was a dramatic reduction in emissions from Eastern Europe and the former Soviet Union. The likelihood that emissions will continue to decline in the future will contribute to future warming. Whereas Stern (2006) uses a combination of previously published data and model estimates, Smith et al. (2011) provide an inventory of sulphur emissions from 1850 to 2005 using a uniform methodology. The results largely confirm Stern’s (2006) findings though the levels are generally lower by a few percent.
References
Houghton, R. A. (2003) Revised estimates of the annual net flux of carbon to the atmosphere from changes in land use and land management 1850-2000, Tellus 55B: 378-390.
Houghton, R. A. (2010) How well do we know the flux of CO2 from land use change? Tellus 62B: 337-351.
Smith, S. J., J. van Ardenne, Z. Klimont, R. J. Andres, A. Volke, S. D. Arias (2011) Anthropogenic sulfur dioxide emissions: 1850-2005, Atmospheric Chemistry and Physics 11: 1101-1116.
Stern D. I. (2005) Beyond the environmental Kuznets curve: Diffusion of sulfur-emissions-abating technology, Journal of Environment and Development 14(1), 101-124.
Stern D. I. (2006) Reversal in the trend of global anthropogenic sulfur emissions, Global Environmental Change 16(2), 207-220.
Stern D. I. and R. K. Kaufmann (1996) Estimates of global anthropogenic methane emissions 1860-1993, Chemosphere 33, 159-176.
Rogelj et al. Mitigation Paper in Nature
The latest issue of Nature has a paper on climate mitigation by Rogelj et al. The issue also has a "News and Views" item by Steve Hatfield Dodds on the paper. The paper has an interesting message*: Delay in acting on mitigation has the biggest effect on the probability of achieving the 2C target, carbon taxes above $20-40 per tonne have little effect on mitigation, and carbon capture and storage (CCS) is essential. This is a message that environmentalists, business, and fossil fuel producers will like. As Steve points out, one weakness of the paper is that it is all done with the MESSAGE integrated assessment model and that is kind of a black box. In the EMF-22 modelling exercise, MESSAGE had some of the lowest carbon taxes. For a 450 ppm scenario its 2020 carbon tax was only $15. By contrast, FUND had a $260 carbon tax. So MESSAGE is an optimistic model. Other models definitely don't have this carbon tax saturation phenomenon as can be seen from our meta-analysis.
Our PhD student Hyung-Sup Lee's PhD thesis will provide a similar kind of uncertainty analysis purely on the economic side of things using that EMF-22 data.
* Pun kind of intended :)
Our PhD student Hyung-Sup Lee's PhD thesis will provide a similar kind of uncertainty analysis purely on the economic side of things using that EMF-22 data.
* Pun kind of intended :)
Wednesday, January 2, 2013
Decomposing Emissions
Latest installment.
The Kaya identity decomposes total energy-related emissions into the product of population, income per capita, energy intensity, and carbon intensity of energy carriers (Kaya, 1997). It is an extension of the IPAT identity (Ehrlich and Holdren, 1971) that decomposes its technology factor into two more factors. It is important to understand that this framework is an accounting identity and not a causal model. For example, growth in income per capita might drive or be associated with reduced energy intensity so that the factors are not independent.
Raupach et al. (2007) is a highly cited example of this literature. They show that global emissions growth since 2000 was driven by a cessation or reversal of earlier declining trends in the energy intensity of gross domestic product (GDP) (energy/GDP) and the carbon intensity of energy (emissions/energy), coupled with continuing increases in population and per-capita GDP. Nearly constant or slightly increasing trends in the carbon intensity of energy were observed in both developed and developing regions and no region was significantly decarbonizing its energy supply. The growth rate in emissions was strongest in rapidly developing economies, particularly China. This research group also published another highly cited paper in 2007 linking emissions growth and its drivers to the atmospheric concentration of carbon dioxide (Canadell et al., 2007).
Many papers examine the role of particular Kaya factors in explaining historical emissions and driving future projections. The most important factor driving declining energy intensity and to some degree carbon intensity is technological change. Grübler et al. (1999) present a framework for energy technology analysis and discuss methods that can be used to analyze the impact of technological changes on global warming. In the historical record, they identify characteristic “learning rates" for the reduction in cost of energy technologies that allow simple quantified characterization of the improvement in cost and performance due to cumulative experience and investments. They also identify patterns, processes and timescales that typify the diffusion of new technologies in competitive markets. Technologies that are long-lived and are components of interlocking networks typically require the longest time to diffuse and co-evolve with other technologies in the network; such network effects yield high barriers to entry even for superior competitors. The authors show how it is possible to include learning phenomena in micro- and macro-scale models. Doing so can yield projections with lessened environmental impacts without necessarily incurring a negative effect on the economy.
The authors also address the final Kaya factor – carbon intensity of energy. They show that over time the fuels that power the economy have had progressively more energy per unit of carbon pollution - from coal to oil to gas. Such replacement has historically “decarbonized'' the global primary energy supply 0.3% per year.
Besides technological change another potential driver of declining energy intensity is structural change of economy towards a service oriented economy. It is usually thought that such an economy will have lower energy intensity and, therefore, emissions intensity of income. Henriques and Kander (2010) argue that this interpretation is overly optimistic because the shift to a service economy is somewhat of an illusion in terms of real production. The share of an industry in the economy is a function of both the real level of production and the price of output. The share of the manufacturing sector has declined in developed countries because rapid productivity gains have reduced its output price relative to the service sector. When constant prices are used, less of a shift to a service economy is seen. The main driver of the decline in energy intensity in developed countries is, therefore, productivity gains in manufacturing. For emerging economies like Brazil, Mexico and India, it is the residential sector that drives energy intensity down because of the declining share of this sector as the formal economy grows, and as a consequence of switching to more efficient fuels.
Another important issue related to the decomposition literature is to what degree trade and foreign investment have allowed developed countries to reduce their apparent energy intensity. Since the early days of the environmental Kuznets curve literature this was seen as a potential explanation of reduced pollution in developed economies (Stern et al., 1996). Most mainstream economists (Levinson, 2010) and economic historians (e.g. Kander and Lindmark 2006) have argued that the role of trade. Peters and Hertwich (2008), however, find that most developed countries were net importers of embodied carbon dioxide emissions in 2001 – in other words, their imports required more emissions to produce than their exports did. For the United States the difference amounted to 120 Mt C while for the UK it was 28 Mt. But this does not imply that if they produced all these products at home their net emissions would be this much higher. This is because production in developing countries is much more energy intensive than in developed countries when measured at market exchange rates and some developed countries, in particular China and India are particularly carbon intensive. This explains the differences on this issue between economists and researchers from engineering backgrounds.
A little researched topic is what happens to the Kaya factors in the short-run over the course of the business cycle. In a response to Peters et al. (2012), Jotzo et al. (2012) hint that the rate of change in energy intensity follows a strong cycle with the rate of decline slowing in the aftermath of recessions and increasing later in the business cycle. Alternatively, emissions could be seen as responding asymmetrically to increases and decreases in income (York, 2012).
References
Canadell, J. G., C. Le Quéré, M. R. Raupach, C. B. Field, E. T. Buitenhuis, P. Ciais, T. J. Conway, N. P. Gillett, R. A. Houghton, and G. Marland (2007) Contributions to accelerating atmospheric CO2 growth from economic activity, carbon intensity, and efficiency of natural sinks, Proceedings of the National Academy of Sciences 104(47): 18866–18870.
Ehrlich, P. R. and J. P. Holdren (1971) Impact of population growth, Science 171(3977): 1212-1217.
Grübler, Arnulf, Nebojsa Nakicénovic, and David G. Victor (1999) Dynamics of energy technologies and global change, Energy Policy 27: 247-280.
Henriques, Sofia Teives, and Astrid Kander (2010) The modest environmental relief resulting from the transition to a service economy, Ecological Economics 70(2): 271-282.
Jotzo F., P. J. Burke, P. J. Wood, A. Macintosh, and D. I. Stern (2012) Decomposing the 2010 global carbon dioxide emissions rebound, Nature Climate Change 2(4): 213-214.
Kander, Astrid and Lindmark, Magnus, 2006. "Foreign trade and declining pollution in Sweden: a decomposition analysis of long-term structural and technological effects," Energy Policy, Elsevier, vol. 34(13), pages 1590-1599, September.
Kaya, Y. and K. Yokobori (1997) Environment, Energy, and Economy: Strategies for Sustainability, United Nations University Press.
Levinson, A. (2010) Offshoring Pollution: Is the United States Increasingly Importing Polluting Goods? Review of Environmental Economics and Policy 4(1): 63-83.
Peters, Glen P. and Edgar G. Hertwich (2008) CO2 Embodied in International Trade with Implications for Global Climate Policy, Environmental Science and Technology 42(5): 1401-1407.
Peters, Glen P., Gregg Marland, Corinne Le Quéré, Thomas Boden, Josep G. Canadell & Michael R. Raupach (2012) Rapid growth in CO2 emissions after the 2008–2009 global financial crisis, Nature Climate Change 2, 2–4.
Raupach, Michael R., Gregg Marland, Philippe Ciais, Corinne Le Quéré, Josep G. Canadell, Gernot Klepper, Christopher B. Field (2007) Global and regional drivers of accelerating CO2 emissions, Proceedings of the National Academy of Sciences 104(24): 10288-10293.
Stern D. I., M. S. Common, and E. B. Barbier (1996) Economic growth and environmental degradation: the environmental Kuznets curve and sustainable development, World Development 24, 1151-1160.
York, R. (2012) Asymmetric effects of economic growth and decline on CO2 emissions, Nature Climate Change 2(11): 762-764.
The Kaya identity decomposes total energy-related emissions into the product of population, income per capita, energy intensity, and carbon intensity of energy carriers (Kaya, 1997). It is an extension of the IPAT identity (Ehrlich and Holdren, 1971) that decomposes its technology factor into two more factors. It is important to understand that this framework is an accounting identity and not a causal model. For example, growth in income per capita might drive or be associated with reduced energy intensity so that the factors are not independent.
Raupach et al. (2007) is a highly cited example of this literature. They show that global emissions growth since 2000 was driven by a cessation or reversal of earlier declining trends in the energy intensity of gross domestic product (GDP) (energy/GDP) and the carbon intensity of energy (emissions/energy), coupled with continuing increases in population and per-capita GDP. Nearly constant or slightly increasing trends in the carbon intensity of energy were observed in both developed and developing regions and no region was significantly decarbonizing its energy supply. The growth rate in emissions was strongest in rapidly developing economies, particularly China. This research group also published another highly cited paper in 2007 linking emissions growth and its drivers to the atmospheric concentration of carbon dioxide (Canadell et al., 2007).
Many papers examine the role of particular Kaya factors in explaining historical emissions and driving future projections. The most important factor driving declining energy intensity and to some degree carbon intensity is technological change. Grübler et al. (1999) present a framework for energy technology analysis and discuss methods that can be used to analyze the impact of technological changes on global warming. In the historical record, they identify characteristic “learning rates" for the reduction in cost of energy technologies that allow simple quantified characterization of the improvement in cost and performance due to cumulative experience and investments. They also identify patterns, processes and timescales that typify the diffusion of new technologies in competitive markets. Technologies that are long-lived and are components of interlocking networks typically require the longest time to diffuse and co-evolve with other technologies in the network; such network effects yield high barriers to entry even for superior competitors. The authors show how it is possible to include learning phenomena in micro- and macro-scale models. Doing so can yield projections with lessened environmental impacts without necessarily incurring a negative effect on the economy.
The authors also address the final Kaya factor – carbon intensity of energy. They show that over time the fuels that power the economy have had progressively more energy per unit of carbon pollution - from coal to oil to gas. Such replacement has historically “decarbonized'' the global primary energy supply 0.3% per year.
Besides technological change another potential driver of declining energy intensity is structural change of economy towards a service oriented economy. It is usually thought that such an economy will have lower energy intensity and, therefore, emissions intensity of income. Henriques and Kander (2010) argue that this interpretation is overly optimistic because the shift to a service economy is somewhat of an illusion in terms of real production. The share of an industry in the economy is a function of both the real level of production and the price of output. The share of the manufacturing sector has declined in developed countries because rapid productivity gains have reduced its output price relative to the service sector. When constant prices are used, less of a shift to a service economy is seen. The main driver of the decline in energy intensity in developed countries is, therefore, productivity gains in manufacturing. For emerging economies like Brazil, Mexico and India, it is the residential sector that drives energy intensity down because of the declining share of this sector as the formal economy grows, and as a consequence of switching to more efficient fuels.
Another important issue related to the decomposition literature is to what degree trade and foreign investment have allowed developed countries to reduce their apparent energy intensity. Since the early days of the environmental Kuznets curve literature this was seen as a potential explanation of reduced pollution in developed economies (Stern et al., 1996). Most mainstream economists (Levinson, 2010) and economic historians (e.g. Kander and Lindmark 2006) have argued that the role of trade. Peters and Hertwich (2008), however, find that most developed countries were net importers of embodied carbon dioxide emissions in 2001 – in other words, their imports required more emissions to produce than their exports did. For the United States the difference amounted to 120 Mt C while for the UK it was 28 Mt. But this does not imply that if they produced all these products at home their net emissions would be this much higher. This is because production in developing countries is much more energy intensive than in developed countries when measured at market exchange rates and some developed countries, in particular China and India are particularly carbon intensive. This explains the differences on this issue between economists and researchers from engineering backgrounds.
A little researched topic is what happens to the Kaya factors in the short-run over the course of the business cycle. In a response to Peters et al. (2012), Jotzo et al. (2012) hint that the rate of change in energy intensity follows a strong cycle with the rate of decline slowing in the aftermath of recessions and increasing later in the business cycle. Alternatively, emissions could be seen as responding asymmetrically to increases and decreases in income (York, 2012).
References
Canadell, J. G., C. Le Quéré, M. R. Raupach, C. B. Field, E. T. Buitenhuis, P. Ciais, T. J. Conway, N. P. Gillett, R. A. Houghton, and G. Marland (2007) Contributions to accelerating atmospheric CO2 growth from economic activity, carbon intensity, and efficiency of natural sinks, Proceedings of the National Academy of Sciences 104(47): 18866–18870.
Ehrlich, P. R. and J. P. Holdren (1971) Impact of population growth, Science 171(3977): 1212-1217.
Grübler, Arnulf, Nebojsa Nakicénovic, and David G. Victor (1999) Dynamics of energy technologies and global change, Energy Policy 27: 247-280.
Henriques, Sofia Teives, and Astrid Kander (2010) The modest environmental relief resulting from the transition to a service economy, Ecological Economics 70(2): 271-282.
Jotzo F., P. J. Burke, P. J. Wood, A. Macintosh, and D. I. Stern (2012) Decomposing the 2010 global carbon dioxide emissions rebound, Nature Climate Change 2(4): 213-214.
Kander, Astrid and Lindmark, Magnus, 2006. "Foreign trade and declining pollution in Sweden: a decomposition analysis of long-term structural and technological effects," Energy Policy, Elsevier, vol. 34(13), pages 1590-1599, September.
Kaya, Y. and K. Yokobori (1997) Environment, Energy, and Economy: Strategies for Sustainability, United Nations University Press.
Levinson, A. (2010) Offshoring Pollution: Is the United States Increasingly Importing Polluting Goods? Review of Environmental Economics and Policy 4(1): 63-83.
Peters, Glen P. and Edgar G. Hertwich (2008) CO2 Embodied in International Trade with Implications for Global Climate Policy, Environmental Science and Technology 42(5): 1401-1407.
Peters, Glen P., Gregg Marland, Corinne Le Quéré, Thomas Boden, Josep G. Canadell & Michael R. Raupach (2012) Rapid growth in CO2 emissions after the 2008–2009 global financial crisis, Nature Climate Change 2, 2–4.
Raupach, Michael R., Gregg Marland, Philippe Ciais, Corinne Le Quéré, Josep G. Canadell, Gernot Klepper, Christopher B. Field (2007) Global and regional drivers of accelerating CO2 emissions, Proceedings of the National Academy of Sciences 104(24): 10288-10293.
Stern D. I., M. S. Common, and E. B. Barbier (1996) Economic growth and environmental degradation: the environmental Kuznets curve and sustainable development, World Development 24, 1151-1160.
York, R. (2012) Asymmetric effects of economic growth and decline on CO2 emissions, Nature Climate Change 2(11): 762-764.
Tuesday, January 1, 2013
Carbon Emissions, The Environmental Kuznets Curve, and Convergence
I'm going to include one paper on the EKC and one on convergence.
The most popular approaches to explaining historical emissions are the environmental Kuznets curve and the decomposition approach using the Kaya identity. These approaches can also be used to produce simple projections of future emissions given information on the relevant drivers.
The environmental Kuznets curve hypothesis proposes that concentrations or per capita emissions of various pollutants rise and then fall as per capita income increases. Static and dynamic theoretical models are given by Plassmann and Khanna (2006) and Brock and Taylor (2010) respectively, while Carson (2010) provides a recent survey. For carbon dioxide the relevant variable is emissions per capita. Following the original paper on the topic by Grossman and Krueger (1991), the World Bank published an issue of the World Development Report timed for the Rio de Janeiro Earth Summit in 1992 that featured an environmental Kuznets curve for carbon dioxide among various environmental indicators. The econometric estimates showed that per capita carbon emissions rise monotonically with per capita income within the observed range (Shafik, 1994). This result was confirmed by Holtz-Eakin and Selden (1995), which is the classic paper on the carbon EKC. They found also found a monotonic relationship between income per capita and CO2 emissions though the propensity to emit with income declines. Recent papers by Wagner (2008), Vollebergh et al. (2009) and Stern (2010) that use different econometric methods do not substantially change the conclusions despite some intervening papers (e.g. Schmalensee et al. 1998) that claimed that there was an inverted U shaped curve for CO2 with an in sample peak. This is also a paper that has stood the test of time in terms of projected emissions to date, though future projected emissions are lower than Edmonds and Reilly (1983) or RCP 8.5.
A related literature looks at whether per capita emissions are converging over time across countries. If there is convergence in GDP per capita then if the income emissions relation is monotonic there should also be convergence in emissions, at least conditionally. Strazicich and List (2003) examined the time paths of carbon dioxide emissions in twenty-one industrial countries from 1960–1997 to test for stochastic and conditional convergence. They performed estimated both panel unit root tests and cross-section regressions. Overall, they found significant evidence that CO2 emissions have converged. Subsequent research has tested whether this result holds across both developed and developing countries with mixed results (e.g. Aldy, 2006; Westerlund and Basher, 2008; Brock and Taylor, 2010).
References
Aldy, Joseph E. (2006) Per capita carbon dioxide emissions: convergence or divergence? Environmental and Resource Economics 33(4): 533-555.
Brock, William A. and M. Scott Taylor (2010) The green Solow model, Journal of Economic Growth 15:127–153.
Carson, R. T. (2010) The environmental Kuznets curve: Seeking empirical regularity and theoretical structure, Review of Environmental Economics and Policy 4(1): 3-23.
Edmonds, Jae and John Reilly (1983) Global energy and CO2 to the year 2050, The Energy Journal 4(3): 21-48.
Grossman, G. M. and A. B. Krueger (1991) Environmental impacts of a North American Free Trade Agreement, National Bureau of Economic Research Working Paper 3914, NBER, Cambridge MA.
Holtz-Eakin, Douglas and Thomas M. Selden (1995) Stoking the fires? CO2 emissions and economic growth, Journal of Public Economics 57(1): 85-101.
Plassmann, Florenz and Neha Khanna (2006) Preferences, Technology, and the Environment: Understanding the Environmental Kuznets Curve Hypothesis, Amer. J. Agr. Econ. 88(3) (August 2006): 632–643.
Schmalensee, R., T. M. Stoker and R. A. Judson (1998), ‘World Carbon Dioxide Emissions: 1950-2050’, Review of Economics and Statistics, 80, 15-27.
Shafik N., Economic development and environmental quality: an econometric analysis, Oxford Economic Papers 46, 757-773 (1994).
Stern D. I. (2010) Between estimates of the emissions-income elasticity, Ecological Economics 69, 2173-2182.
Strazicich, Mark C. and John A. List (2003) Are CO2 emission levels converging among industrial countries? Environmental and Resource Economics 24(3): 263-271.
Vollebergh, Herman R.J., Bertrand Melenberg, and Elbert Dijkgraaf (2009) Identifying reduced-form relations with panel data: The case of pollution and income, Journal of Environmental Economics and Management 58(1): 27-42.
Wagner, M., 2008. The carbon Kuznets curve: A cloudy picture emitted by bad econometrics. Resource and Energy Economics 30, 388-408.
Westerlund, Joakim and Syed A. Basher (2008) Testing for convergence in carbon dioxide emissions using a century of panel data, Environmental and Resource Economics 40:109–120.
The most popular approaches to explaining historical emissions are the environmental Kuznets curve and the decomposition approach using the Kaya identity. These approaches can also be used to produce simple projections of future emissions given information on the relevant drivers.
The environmental Kuznets curve hypothesis proposes that concentrations or per capita emissions of various pollutants rise and then fall as per capita income increases. Static and dynamic theoretical models are given by Plassmann and Khanna (2006) and Brock and Taylor (2010) respectively, while Carson (2010) provides a recent survey. For carbon dioxide the relevant variable is emissions per capita. Following the original paper on the topic by Grossman and Krueger (1991), the World Bank published an issue of the World Development Report timed for the Rio de Janeiro Earth Summit in 1992 that featured an environmental Kuznets curve for carbon dioxide among various environmental indicators. The econometric estimates showed that per capita carbon emissions rise monotonically with per capita income within the observed range (Shafik, 1994). This result was confirmed by Holtz-Eakin and Selden (1995), which is the classic paper on the carbon EKC. They found also found a monotonic relationship between income per capita and CO2 emissions though the propensity to emit with income declines. Recent papers by Wagner (2008), Vollebergh et al. (2009) and Stern (2010) that use different econometric methods do not substantially change the conclusions despite some intervening papers (e.g. Schmalensee et al. 1998) that claimed that there was an inverted U shaped curve for CO2 with an in sample peak. This is also a paper that has stood the test of time in terms of projected emissions to date, though future projected emissions are lower than Edmonds and Reilly (1983) or RCP 8.5.
A related literature looks at whether per capita emissions are converging over time across countries. If there is convergence in GDP per capita then if the income emissions relation is monotonic there should also be convergence in emissions, at least conditionally. Strazicich and List (2003) examined the time paths of carbon dioxide emissions in twenty-one industrial countries from 1960–1997 to test for stochastic and conditional convergence. They performed estimated both panel unit root tests and cross-section regressions. Overall, they found significant evidence that CO2 emissions have converged. Subsequent research has tested whether this result holds across both developed and developing countries with mixed results (e.g. Aldy, 2006; Westerlund and Basher, 2008; Brock and Taylor, 2010).
References
Aldy, Joseph E. (2006) Per capita carbon dioxide emissions: convergence or divergence? Environmental and Resource Economics 33(4): 533-555.
Brock, William A. and M. Scott Taylor (2010) The green Solow model, Journal of Economic Growth 15:127–153.
Carson, R. T. (2010) The environmental Kuznets curve: Seeking empirical regularity and theoretical structure, Review of Environmental Economics and Policy 4(1): 3-23.
Edmonds, Jae and John Reilly (1983) Global energy and CO2 to the year 2050, The Energy Journal 4(3): 21-48.
Grossman, G. M. and A. B. Krueger (1991) Environmental impacts of a North American Free Trade Agreement, National Bureau of Economic Research Working Paper 3914, NBER, Cambridge MA.
Holtz-Eakin, Douglas and Thomas M. Selden (1995) Stoking the fires? CO2 emissions and economic growth, Journal of Public Economics 57(1): 85-101.
Plassmann, Florenz and Neha Khanna (2006) Preferences, Technology, and the Environment: Understanding the Environmental Kuznets Curve Hypothesis, Amer. J. Agr. Econ. 88(3) (August 2006): 632–643.
Schmalensee, R., T. M. Stoker and R. A. Judson (1998), ‘World Carbon Dioxide Emissions: 1950-2050’, Review of Economics and Statistics, 80, 15-27.
Shafik N., Economic development and environmental quality: an econometric analysis, Oxford Economic Papers 46, 757-773 (1994).
Stern D. I. (2010) Between estimates of the emissions-income elasticity, Ecological Economics 69, 2173-2182.
Strazicich, Mark C. and John A. List (2003) Are CO2 emission levels converging among industrial countries? Environmental and Resource Economics 24(3): 263-271.
Vollebergh, Herman R.J., Bertrand Melenberg, and Elbert Dijkgraaf (2009) Identifying reduced-form relations with panel data: The case of pollution and income, Journal of Environmental Economics and Management 58(1): 27-42.
Wagner, M., 2008. The carbon Kuznets curve: A cloudy picture emitted by bad econometrics. Resource and Energy Economics 30, 388-408.
Westerlund, Joakim and Syed A. Basher (2008) Testing for convergence in carbon dioxide emissions using a century of panel data, Environmental and Resource Economics 40:109–120.
Most Popular Posts 2012
These are the most popular new posts in 2012. In general my readers are interested in journal rankings and impact and jobs but also some other topics. These numbers are based on my Google Analytics reports. The stats that Google now provides within Blogger would give a somewhat different hit list.
1. PLOS One's 2011 Impact Factor. PLoS ONE is the world's biggest journal and so a lot of people are interested in its impact factor. A lot of the hits on my blog are PLoS ONE related.
2. In Defence of Elsevier. Being controversial helps hits :)
3. Several Crawford Jobs Available. I posted the link on RESECON and got lots of hits.
4. The Rise and Fall of Ecological Economics. This is more of a surprise in terms of number of hits.
5. Scientific Collaboration Networks. These maps are cool.
6. 2011 Journal Citation Report Released. More journal rankings.
7. Acceptance Rates in the Top Environmental Economics Journals. More on getting published, or not.
8. Google Scholar Metrics. Another way to rank journals.
9. Calculating an Individual Impact Factor Using Scopus. A way to compare individual researchers to journals. And it is pretty easy to do.
10. The Inside Story on the 2010 ERA Economics Journals Rankings. Yet more on journal rankings.
1. PLOS One's 2011 Impact Factor. PLoS ONE is the world's biggest journal and so a lot of people are interested in its impact factor. A lot of the hits on my blog are PLoS ONE related.
2. In Defence of Elsevier. Being controversial helps hits :)
3. Several Crawford Jobs Available. I posted the link on RESECON and got lots of hits.
4. The Rise and Fall of Ecological Economics. This is more of a surprise in terms of number of hits.
5. Scientific Collaboration Networks. These maps are cool.
6. 2011 Journal Citation Report Released. More journal rankings.
7. Acceptance Rates in the Top Environmental Economics Journals. More on getting published, or not.
8. Google Scholar Metrics. Another way to rank journals.
9. Calculating an Individual Impact Factor Using Scopus. A way to compare individual researchers to journals. And it is pretty easy to do.
10. The Inside Story on the 2010 ERA Economics Journals Rankings. Yet more on journal rankings.