Henry D. Jacoby
Massachusetts Institute of Technology
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Featured researches published by Henry D. Jacoby.
Nature | 1999
John M. Reilly; Ronald G. Prinn; Jochen Harnisch; Jean. Fitzmaurice; Henry D. Jacoby; David W. Kicklighter; Peter H. Stone; Andrei P. Sokolov; Chien Wang
The Kyoto Protocol allows reductions in emissions of several ‘greenhouse’ gases to be credited against a CO2-equivalent emissions limit, calculated using ‘global warming potential’ indices for each gas. Using an integrated global-systems model, it is shown that a multi-gas control strategy could greatly reduce the costs of fulfilling the Kyoto Protocol compared with a CO2-only strategy. Extending the Kyoto Protocol to 2100 without more severe emissions reductions shows little difference between the two strategies in climate and ecosystem effects. Under a more stringent emissions policy, the use of global warming potentials as applied in the Kyoto Protocol leads to considerably more mitigation of climate change for multi-gas strategies than for the—supposedly equivalent—CO2-only control, thus emphasizing the limits of global warming potentials as a tool for political decisions.
Energy Policy | 2004
Henry D. Jacoby; A. Denny Ellerman
Abstract The “safety valve” is a possible addition to a cap-and-trade system of emissions regulation whereby the authority offers to sell permits in unlimited amount at a pre-set price. In this way the cost of meeting the cap can be limited. It was proposed in the US as a way to control perceived high costs of the Kyoto Protocol, and possibly as a way to shift the focus of policy from the quantity targets of the Protocol to emissions price. In international discussions, the idea emerged as a proposal for a compliance penalty. The usefulness of the safety valve depends on the conditions under which it might be introduced. For a time it might tame an overly stringent emissions target. It also can help control the price volatility during the introduction of gradually tightening one, although permit banking can ultimately serve the same function. It is unlikely to serve as a long-term feature of a cap-and-trade system, however, because of the complexity of coordinating price and quantity instruments and because it will interfere with the development of systems of international emissions trade.
Journal of Climate | 2009
Andrei P. Sokolov; Peter H. Stone; Chris E. Forest; Ronald G. Prinn; Marcus C. Sarofim; Mort Webster; Sergey Paltsev; Courtney Adam Schlosser; David W. Kicklighter; Stephanie Dutkiewicz; John M. Reilly; Chien Wang; Benjamin S. Felzer; Jerry M. Melillo; Henry D. Jacoby
Abstract The Massachusetts Institute of Technology (MIT) Integrated Global System Model is used to make probabilistic projections of climate change from 1861 to 2100. Since the model’s first projections were published in 2003, substantial improvements have been made to the model, and improved estimates of the probability distributions of uncertain input parameters have become available. The new projections are considerably warmer than the 2003 projections; for example, the median surface warming in 2091–2100 is 5.1°C compared to 2.4°C in the earlier study. Many changes contribute to the stronger warming; among the more important ones are taking into account the cooling in the second half of the twentieth century due to volcanic eruptions for input parameter estimation and a more sophisticated method for projecting gross domestic product (GDP) growth, which eliminated many low-emission scenarios. However, if recently published data, suggesting stronger twentieth-century ocean warming, are used to determine...
Climatic Change | 1999
Ronald G. Prinn; Henry D. Jacoby; Andrei P. Sokolov; Chien Wang; Xiangming Xiao; Zonggui Yang; R. Eckhaus; Peter H. Stone; D. Ellerman; Jerry M. Melillo; J. Fitzmaurice; David W. Kicklighter; Gary L. Holian; Yunzhi Liu
Alternative policies to address global climate change are being debated in many nations and within the United Nations Framework Convention on Climate Change. To help provide objective and comprehensive analyses in support of this process, we have developed a model of the global climate system consisting of coupled sub-models of economic growth and associated emissions, natural fluxes, atmospheric chemistry, climate, and natural terrestrial ecosystems. The framework of this Integrated Global System Model is described and the results of sample runs and a sensitivity analysis are presented. This multi-component model addresses most of the major anthropogenic and natural processes involved in climate change and also is computationally efficient. As such, it can be used effectively to study parametric and structural uncertainty and to analyze the costs and impacts of many policy alternatives. Initial runs of the model have helped to define and quantify a number of feedbacks among the sub-models, and to elucidate the geographical variations in several variables that are relevant to climate science and policy. The effect of changes in climate and atmospheric carbon dioxide levels on the uptake of carbon and emissions of methane and nitrous oxide by land ecosystems is one potentially important feedback which has been identified. The sensitivity analysis has enabled preliminary assessment of the effects of uncertainty in the economic, atmospheric chemistry, and climate sub-models as they influence critical model results such as predictions of temperature, sea level, rainfall, and ecosystem productivity. We conclude that uncertainty regarding economic growth, technological change, deep oceanic circulation, aerosol radiative forcing, and cloud processes are important influences on these outputs.
Environmental Modeling & Assessment | 2003
Robert C. Hyman; John M. Reilly; Mustafa H. Babiker; Ardoin. De Masin; Henry D. Jacoby
Although emissions of CO2 are the largest anthropogenic contributor to the risks of climate change, other substances are important in the formulation of a cost-effective response. To provide improved facilities for addressing their role, we develop an approach for endogenizing control of these other greenhouse gases within a computable general equilibrium (CGE) model of the world economy. The calculation is consistent with underlying economic production theory. For parameterization it is able to draw on marginal abatement cost (MAC) functions for these gases based on detailed technological descriptions of control options. We apply the method to the gases identified in the Kyoto Protocol: methane (CH4), nitrous oxide (N2O), sulfur hexaflouride (SF6), the perflourocarbons (PFCs), and the hydrofluorocarbons (HFCs). Complete and consistent estimates are provided of the costs of meeting greenhouse-gas reduction targets with a focus on “what” flexibility – i.e., the ability to abate the most cost-effective mix of gases in any period. We find that non-CO2 gases are a crucial component of a cost-effective policy. Because of their high GWPs under current international agreements they would contribute a substantial share of early abatement.
Climate Policy | 2008
Sergey Paltsev; John M. Reilly; Henry D. Jacoby; Angelo Costa Gurgel; Gilbert E. Metcalf; Andrei P. Sokolov; Jennifer F. Holak
In 2007 the US Congress began considering a set of bills to implement a cap-and-trade system to limit the nations greenhouse gas (GHG) emissions. The MIT Integrated Global System Model (IGSM)—and its economic component, the Emissions Prediction and Policy Analysis (EPPA) model—were used to assess these proposals. In the absence of policy, the EPPA model projects a doubling of US greenhouse gas emissions by 2050. Global emissions, driven by growth in developing countries, are projected to increase even more. Unrestrained, these emissions would lead to an increase in global CO2 concentration from a current level of 380 ppmv to about 550 ppmv by 2050 and to near 900 ppmv by 2100, resulting in a year 2100 global temperature 3.5–4.5°C above the current level. The more ambitious of the Congressional proposals could limit this increase to around 2°C, but only if other nations, including developing countries, also strongly controlled greenhouse gas emissions. With these more aggressive reductions, the economic cost measured in terms of changes in total welfare in the United States could range from 1.5% to almost 2% by the 2040–2050 period, with 2015 CO2-equivalent prices between
Financial Management | 1993
David G. Laughton; Henry D. Jacoby
30 and
Energy Policy | 2000
Mustafa H.M. Babiker; John M. Reilly; Henry D. Jacoby
55, rising to between
Climatic Change | 2012
Mort Webster; Andrei P. Sokolov; John M. Reilly; Chris E. Forest; Sergey Paltsev; Adam Schlosser; Chien Wang; David W. Kicklighter; Marcus C. Sarofim; Jerry M. Melillo; Ronald G. Prinn; Henry D. Jacoby
120 and
Foreign Affairs | 1998
Henry D. Jacoby; Ronald G. Prinn; Richard Schmalensee
210 by 2050. This level of cost would not seriously affect US GDP growth but would imply large-scale changes in its energy system.