The 2013 ANZSEE Conference will take place in November at the Crawford School. All abstracts are due by 26th July. There will both be traditional papers and "working groups" that sound something like panel discussions. The last ANZSEE conference went to was the ANZSEE Conference in Darwin in 2009, which I thought was a great conference. The last ANZSEE or ISEE conference in Canberra was the 2000 ISEE Conference.
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.
Monday, December 31, 2012
Scenarios and Forecasts of CO2 Emissions
Today's installment. This is another four papers, marked in bold the first time they appear. I can see already that either I am going to have to cut the number of papers covered or we are going to have to go to two volumes, which is an option. Also, I gave up and actually included an IPCC report in my list.
******
Economists first addressed the issue of climate change as part of the wave of interest in energy and environmental economics that followed the oil price shock in 1973-4. The first journal article on the issue is d’Arge et al. (1982), which references an earlier report (d’Arge et al., 1975) and conference paper by the authors.
Early scenarios and projections for future emissions of carbon dioxide were published the following year (Nordhaus and Yohe, 1983; Ausubel and Nordhaus, 1983; Edmonds and Reilly 1983). Edmonds and Reilly’s model was the basis of the energy module of the later IS92 scenarios. It consists of a multiregional supply and demand model for seven primary and secondary energy carriers. Aggregate energy demand is determined by GNP, which is driven by exogenous technological change, and autonomous energy efficiency improvements for each fuel type. There is also a feedback from energy prices to GNP. Predicted carbon emissions rose to 6.9 billion tonnes in 2000, 12.3 billion in 2025 and 26 billion by 2050 with an increasing share of emissions in the non-OECD world. The near-term prediction was remarkably accurate - actual global emissions were 6.8 billion tonnes in 2000. Predicted emissions for 2050 are higher than current BAU projections as we will see below. Carbon dioxide concentrations were predicted to double between 2049 and 2067 relative to the preindustrial level, which is in line with current BAU projections.
Many of the most important studies of future emissions have been published as reports of the Intergovernmental Panel on Climate Change (IPCC) and other agencies. The IPCC has commissioned emissions scenarios roughly every decade – the IS92 scenarios (Leggett et al., 1992), SRES scenarios (Nakicenovic et al., 2000), and RCP scenarios (van Vuuren et al., 2011).
The first IPCC scenarios were produced in 1989. Due to the ending of communism in the USSR and Eastern Europe, the signing of an international agreement on the control of CFCs and new information in various input variables, the IPCC requested a revision only two years later (Leggett et al., 1992). These new scenarios were inputs to the 1992 Supplementary Report and the 1995 Second Assessment Report. These were the first scenarios to include the full suite of greenhouse gases as well as sulphur emissions (Nakicenovic, 2000). In addition to the energy module described above there are deforestation, agriculture, and halocarbon emission modules. Control of sulphur emissions is modelled as an increasing function of income level and an atmosphere/ocean module translates emissions into climate change. The scenarios modelled six alternative future worlds and comprehensively covered all sources of greenhouse gases translating them into CO2 equivalents. Scenarios varied on assumed population and economic growth and the availability of alternative energy technologies and fossil fuel resources. These scenarios result in a very broad range of emissions trajectories. IS92e saw emissions rising to the 20 GT range around 2050 and the 35 GT by 2100. IS92c predicted that emissions would decline after 2020. The preferred scenario, IS92a, was midway between these extremes with emissions around 20 GT in 2100.
The SRES scenarios prepared for the Third Assessment Report (Nakicenovic et al., 2000) are perhaps the best known of the IPCC scenarios. Nakicenovic (2000) discusses the development of these scenarios. Four storylines were developed which vary by population and economic growth, degree of international cooperation and trade, the rate of technological development, and the types of future policies. Five integrated assessment modeling groups cooperated to develop a total of forty scenarios based on the storylines. The results from one of the modeling groups was considered the representative or “marker” scenario of the storyline. The ensemble of results portray greater radiative forcing than the IS92 scenarios mainly because of reduced forecasts of sulfur emissions. The marker A1 and A2 scenarios also project less carbon emissions in 2050 than Edmonds and Reilly (1983).
van Vuuren et al., (2011) introduce the latest IPCC scenarios known as the Representative Concentration Pathways (RCP) prepared for the Fifth Assessment Report. This process is the reverse of previous scenario-building exercises as it starts with concentration pathways based on given radiative forcing targets and then works back to socio-economic scenarios that could lead to those outcomes. These pathways were supposed to be representative of the range of scenarios in the literature and are named for the level of radiative forcing in Watts per square metre in 2100. The RCP 8.5 and 6.0 scenarios might be seen as business as usual under more or less optimistic assumptions about technological change while the RCP 4.5 and 2.6 scenarios assume policy to control emissions. The RCP 2.6 scenario results in negative emissions in the second half of the 21st century which is only possible with biomass carbon capture and storage or air capture of carbon dioxide. Emissions under the RCP 8.5 scenario track those in Edmonds and Reilly (1983) while they are lower in the other scenarios.
References
Ausubel, J. H. & W. D. Nordhaus (1983) A review of estimates of future carbon dioxide emissions, in T. F. Malone (ed.) Changing Climate: Report of the Carbon Dioxide Assessment Committee, National Academy Press, Washington DC. Chapter 2.2 pp153-185.
d’Arge, R. C. et al. (1975) Economic and Social Measures of Biologic and Climatic Change, U.S. Department of Transportation.
d'Arge, Ralph C., William D. Schulze, and David S. Brookshire (1982) Carbon dioxide and intergenerational choice, American Economic Review 72(2): 251-256.
Edmonds, Jae and John Reilly (1983) Global energy and CO2 to the year 2050, The Energy Journal 4(3): 21-48.
Leggett, J., W. J. Pepper, and R. J. Swart (1992) Emissions scenarios for the IPCC: an update, in: J. T. Houghton, B. A. Callander, and S. K. Varney (eds.) Climate Change 1992: The Supplementary Report to the IPCC Scientific Assessment, Cambridge University Press. Chapter A3, 69-96.
Nakićenović, Nebojša (2000) Greenhouse gas emissions scenarios, Technological Forecasting and Social Change 65(2): 149–166.
Nakicenovic, Nebojsa et al. (2000) Special Report on Emissions Scenarios: A Special Report of Working Group III of the Intergovernmental Panel on Climate Change, Cambridge University Press.
Nordhaus, W. D. and G. W. Yohe (1983) Future paths of energy and carbon dioxide emissions, in T. F. Malone (ed.) Changing Climate: Report of the Carbon Dioxide Assessment Committee, National Academy Press, Washington DC. Chapter 2.1, pp87-152.
van Vuuren, Detlef P., Jae Edmonds, Mikiko Kainuma, Keywan Riahi, Allison Thomson, Kathy Hibbard, George C. Hurtt, Tom Kram, Volker Krey, Jean-Francois Lamarque, Toshihiko Masui, Malte Meinshausen, Nebojsa Nakicenovic, Steven J. Smith, and Steven K. Rose (2011) The representative concentration pathways: an overview, Climatic Change 109(1-2): 5-31.
******
Economists first addressed the issue of climate change as part of the wave of interest in energy and environmental economics that followed the oil price shock in 1973-4. The first journal article on the issue is d’Arge et al. (1982), which references an earlier report (d’Arge et al., 1975) and conference paper by the authors.
Early scenarios and projections for future emissions of carbon dioxide were published the following year (Nordhaus and Yohe, 1983; Ausubel and Nordhaus, 1983; Edmonds and Reilly 1983). Edmonds and Reilly’s model was the basis of the energy module of the later IS92 scenarios. It consists of a multiregional supply and demand model for seven primary and secondary energy carriers. Aggregate energy demand is determined by GNP, which is driven by exogenous technological change, and autonomous energy efficiency improvements for each fuel type. There is also a feedback from energy prices to GNP. Predicted carbon emissions rose to 6.9 billion tonnes in 2000, 12.3 billion in 2025 and 26 billion by 2050 with an increasing share of emissions in the non-OECD world. The near-term prediction was remarkably accurate - actual global emissions were 6.8 billion tonnes in 2000. Predicted emissions for 2050 are higher than current BAU projections as we will see below. Carbon dioxide concentrations were predicted to double between 2049 and 2067 relative to the preindustrial level, which is in line with current BAU projections.
Many of the most important studies of future emissions have been published as reports of the Intergovernmental Panel on Climate Change (IPCC) and other agencies. The IPCC has commissioned emissions scenarios roughly every decade – the IS92 scenarios (Leggett et al., 1992), SRES scenarios (Nakicenovic et al., 2000), and RCP scenarios (van Vuuren et al., 2011).
The first IPCC scenarios were produced in 1989. Due to the ending of communism in the USSR and Eastern Europe, the signing of an international agreement on the control of CFCs and new information in various input variables, the IPCC requested a revision only two years later (Leggett et al., 1992). These new scenarios were inputs to the 1992 Supplementary Report and the 1995 Second Assessment Report. These were the first scenarios to include the full suite of greenhouse gases as well as sulphur emissions (Nakicenovic, 2000). In addition to the energy module described above there are deforestation, agriculture, and halocarbon emission modules. Control of sulphur emissions is modelled as an increasing function of income level and an atmosphere/ocean module translates emissions into climate change. The scenarios modelled six alternative future worlds and comprehensively covered all sources of greenhouse gases translating them into CO2 equivalents. Scenarios varied on assumed population and economic growth and the availability of alternative energy technologies and fossil fuel resources. These scenarios result in a very broad range of emissions trajectories. IS92e saw emissions rising to the 20 GT range around 2050 and the 35 GT by 2100. IS92c predicted that emissions would decline after 2020. The preferred scenario, IS92a, was midway between these extremes with emissions around 20 GT in 2100.
The SRES scenarios prepared for the Third Assessment Report (Nakicenovic et al., 2000) are perhaps the best known of the IPCC scenarios. Nakicenovic (2000) discusses the development of these scenarios. Four storylines were developed which vary by population and economic growth, degree of international cooperation and trade, the rate of technological development, and the types of future policies. Five integrated assessment modeling groups cooperated to develop a total of forty scenarios based on the storylines. The results from one of the modeling groups was considered the representative or “marker” scenario of the storyline. The ensemble of results portray greater radiative forcing than the IS92 scenarios mainly because of reduced forecasts of sulfur emissions. The marker A1 and A2 scenarios also project less carbon emissions in 2050 than Edmonds and Reilly (1983).
van Vuuren et al., (2011) introduce the latest IPCC scenarios known as the Representative Concentration Pathways (RCP) prepared for the Fifth Assessment Report. This process is the reverse of previous scenario-building exercises as it starts with concentration pathways based on given radiative forcing targets and then works back to socio-economic scenarios that could lead to those outcomes. These pathways were supposed to be representative of the range of scenarios in the literature and are named for the level of radiative forcing in Watts per square metre in 2100. The RCP 8.5 and 6.0 scenarios might be seen as business as usual under more or less optimistic assumptions about technological change while the RCP 4.5 and 2.6 scenarios assume policy to control emissions. The RCP 2.6 scenario results in negative emissions in the second half of the 21st century which is only possible with biomass carbon capture and storage or air capture of carbon dioxide. Emissions under the RCP 8.5 scenario track those in Edmonds and Reilly (1983) while they are lower in the other scenarios.
References
Ausubel, J. H. & W. D. Nordhaus (1983) A review of estimates of future carbon dioxide emissions, in T. F. Malone (ed.) Changing Climate: Report of the Carbon Dioxide Assessment Committee, National Academy Press, Washington DC. Chapter 2.2 pp153-185.
d’Arge, R. C. et al. (1975) Economic and Social Measures of Biologic and Climatic Change, U.S. Department of Transportation.
d'Arge, Ralph C., William D. Schulze, and David S. Brookshire (1982) Carbon dioxide and intergenerational choice, American Economic Review 72(2): 251-256.
Edmonds, Jae and John Reilly (1983) Global energy and CO2 to the year 2050, The Energy Journal 4(3): 21-48.
Leggett, J., W. J. Pepper, and R. J. Swart (1992) Emissions scenarios for the IPCC: an update, in: J. T. Houghton, B. A. Callander, and S. K. Varney (eds.) Climate Change 1992: The Supplementary Report to the IPCC Scientific Assessment, Cambridge University Press. Chapter A3, 69-96.
Nakićenović, Nebojša (2000) Greenhouse gas emissions scenarios, Technological Forecasting and Social Change 65(2): 149–166.
Nakicenovic, Nebojsa et al. (2000) Special Report on Emissions Scenarios: A Special Report of Working Group III of the Intergovernmental Panel on Climate Change, Cambridge University Press.
Nordhaus, W. D. and G. W. Yohe (1983) Future paths of energy and carbon dioxide emissions, in T. F. Malone (ed.) Changing Climate: Report of the Carbon Dioxide Assessment Committee, National Academy Press, Washington DC. Chapter 2.1, pp87-152.
van Vuuren, Detlef P., Jae Edmonds, Mikiko Kainuma, Keywan Riahi, Allison Thomson, Kathy Hibbard, George C. Hurtt, Tom Kram, Volker Krey, Jean-Francois Lamarque, Toshihiko Masui, Malte Meinshausen, Nebojsa Nakicenovic, Steven J. Smith, and Steven K. Rose (2011) The representative concentration pathways: an overview, Climatic Change 109(1-2): 5-31.
My Year in Review 2012
This year was not quite as eventful as last - it was mainly a case of following through with things started or planned last year - but there is plenty to report.
In January I took over as Research Director in the Crawford School a role that covers both research related administration and leadership and being director of PhD study in the School. One of my first tasks was contributing to ANU's ERA 2012 submission. We were happy to see that our efforts and those of all the researchers that we were reporting on were rewarded with an improvement in ANU's score in economics compared to 2010. There were other big developments in Crawford's Research Profile over the year. CAMA moved to the Crawford School from the College of Business, which boosted Crawford's RePEc ranking in Australia to the top 5. We have made several other appointments and most importantly hired Bob Costanza to one of the Public Policy Chairs. Warwick McKibbin who moved to Crawford with CAMA in August was the first. Bob is the most cited person at ANU on Google Scholar Citations. Bob and Ida Kubiszewski have been visiting Crawford since August.
Old Canberra House, Crawford School, ANU
My role as PhD director took up more of my time but mostly it is a case of improving policies and processes and moving students through the milestones of the PhD. It's good that I have a great team working with me. I couldn't possibly do the job without the help of Robyn Walter who is our PhD administrator. I was also helped by PhD convenors in economics - Amy Liu, in policy and governance - Andy Kennedy, and Colin Filer for economics. Last and definitely not least is Megan Poore who has been acting PhD academic skills adviser since May. Megan has done a really great job working with PhD students one and one and in workshops and courses and steered the first year students committee in putting on our annual PhD Conference.
I published five papers this year. The paper in the Journal of Economic Surveys on interfuel substitution had been "in press" since 2010 but was finally included in a formal journal issue this year. I think we will be seeing fewer of these long gestations in the future. My other single author paper - on energy efficiency trends - was only in press since March. I first submitted it in 2010 though. I also published three papers with co-authors. A paper on the costs of reducing carbon emissions with Jack Pezzey published in AJARE, my first paper with Astrid Kander using long-run historical energy and growth data, and a short piece with four other ANU coauthors on decomposing the steep rise in global carbon emissions in 2010 in Nature Climate Change. The paper with Astrid was also my first successful publication in the Energy Journal. My chapter in the Encyclopedia of Environmetrics on ecological economics was also officially published and we had two articles published on The Conversation.

In January I took over as Research Director in the Crawford School a role that covers both research related administration and leadership and being director of PhD study in the School. One of my first tasks was contributing to ANU's ERA 2012 submission. We were happy to see that our efforts and those of all the researchers that we were reporting on were rewarded with an improvement in ANU's score in economics compared to 2010. There were other big developments in Crawford's Research Profile over the year. CAMA moved to the Crawford School from the College of Business, which boosted Crawford's RePEc ranking in Australia to the top 5. We have made several other appointments and most importantly hired Bob Costanza to one of the Public Policy Chairs. Warwick McKibbin who moved to Crawford with CAMA in August was the first. Bob is the most cited person at ANU on Google Scholar Citations. Bob and Ida Kubiszewski have been visiting Crawford since August.
Old Canberra House, Crawford School, ANU
My role as PhD director took up more of my time but mostly it is a case of improving policies and processes and moving students through the milestones of the PhD. It's good that I have a great team working with me. I couldn't possibly do the job without the help of Robyn Walter who is our PhD administrator. I was also helped by PhD convenors in economics - Amy Liu, in policy and governance - Andy Kennedy, and Colin Filer for economics. Last and definitely not least is Megan Poore who has been acting PhD academic skills adviser since May. Megan has done a really great job working with PhD students one and one and in workshops and courses and steered the first year students committee in putting on our annual PhD Conference.
I published five papers this year. The paper in the Journal of Economic Surveys on interfuel substitution had been "in press" since 2010 but was finally included in a formal journal issue this year. I think we will be seeing fewer of these long gestations in the future. My other single author paper - on energy efficiency trends - was only in press since March. I first submitted it in 2010 though. I also published three papers with co-authors. A paper on the costs of reducing carbon emissions with Jack Pezzey published in AJARE, my first paper with Astrid Kander using long-run historical energy and growth data, and a short piece with four other ANU coauthors on decomposing the steep rise in global carbon emissions in 2010 in Nature Climate Change. The paper with Astrid was also my first successful publication in the Energy Journal. My chapter in the Encyclopedia of Environmetrics on ecological economics was also officially published and we had two articles published on The Conversation.

So far for 2013, I have one paper in press (see below) and a revise and resubmit. I only put out one working paper in 2012. There are lots of partly finished papers that we need to make progress on over the next couple of months. I have discussed or hinted at some of these ideas on this blog. I'll report on them in detail as they are gradually finalized.
Work began on the research funded by the ARC grant we were awarded last year. The most important activities this year have been Astrid Kander's visit to Canberra to collaborate on the project - writing a couple of those unfinished papers - and the search for a post-doctoral research fellow. We got a strong response to the advertisement (mainly through RESECON) and recently interviewed some candidates and are in the process of making an offer.
Earlier in the year, Stephan Bruns and Christian Gross visited Canberra. Stephan spent most of June working with me and I then went to the IAEE meeting in Perth and met up with Christian who then came to Canberra for a day before going on to the Schumpeter conference in Brisbane. We have several unfinished papers in progress :)
In addition to the IAEE meeting in June, I also participated in the MAER meta-analysis in economics workshop in Perth in September. They were the only two conferences I went to in 2012. I'm not a big conference-goer. I gave a couple of invited seminars. One at University of Western Australia and the other at Wirtschaftsuniversität Wien.
I went on two international trips driven by the IPCC Working Group III meetings in Wellington, NZ and Vigo, Spain. The first meeting was to progress from the so-called zero-order draft of the 5th Assessment Report to the first-order draft which was then opened to comments by reviewers. At the Vigo meeting we began the response to these comments and the views of the co-chairs on how the draft needs to change. The final meeting for us will be in Ethiopia next July. I took the opportunity for further travel before the NZ meeting and after the meeting in Spain.
Mount Ruapehu, North Island, NZ
On the teaching front, I taught a new course - Energy Economics - in the second semester. Based on the student evaluations, it was a great success. They especially liked the guest lectures I organized by Chris Short, Hugh Saddler, Paul Burke, and Astrid Kander.
I also again taught an introductory microeconomics course - Economic Way of Thinking I and gave a series of three lectures in our flagship CRWF 8000 course in each semester as well as a few guest lectures.
Finally, I also do a lot of refereeing and editing work... In my role as associate editor of Ecological Economics. I was involved in the dispute between Tol and Ackerman resulting in the posting of comments by me and them in the journal.
Things lined up for 2013 include a visit to Ethiopia and a paper in the March issue of the Journal of Economic Literature.
Tomorrow there'll be a post on the most popular blogposts of 2012.
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