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In this paper we examine the interaction between technology policy and its impact on the full basket of worldwide greenhouse emissions over the 21st century. The heart of the analysis is the Argonne National Laboratory's AMIGA Modeling System, a technology rich, general equilibrium model that (depending on data availability) characterizes as many as 200 sectors of the regional economies. We suggest in this paper that technologies and technology policies exist which could reduce carbon emissions enough to achieve stabilization targets at relatively modest costs given the size of the world economy. This can be accomplished largely through harnessing market forces and creating incentives with the use of efficient prices on greenhouse gas emissions, combined with complementary programs and policies to reduce market failures and to promote new technology improvements and investments. [ABSTRACT FROM AUTHOR]

To address the problem of human induced climate change effectively, climate policy must embody the principles of economic efficiency, environmental effectiveness and equity. In this paper it is shown that such a climate change policy should include a broad coverage of major greenhouse gases and sources. ABARE's Global Trade and Environment Model (GTEM) is used to analyse the economic impact of meeting a radiative forcing target using policies that focus on carbon dioxide emissions only and policies that focus on all major greenhouse gases and sources, including land use change and forestry emissions. It is projected that incorporating non-carbon dioxide gases into climate change policy reduces the economic adjustment cost significantly. Broadening the sources of carbon dioxide to include land use change and forestry emissions further reduces the economic adjustment costs. [ABSTRACT FROM AUTHOR]

This paper examines the role of climate forcing agents other than carbon dioxide using the MiniCAM integrated assessment model for both no-climate-policy and policy emissions scenarios. Non-CO2 greenhouse-gas forcing is dominated by methane and tropospheric ozone. Assumptions about the prevalence of methane recovery and local air pollution controls in the no-policy cases are a critical determinant of methane and ozone-precursor emissions. When these factors are considered, emissions are substantially reduced relative to earlier estimates. This reduces their potential as climate mitigation agents through specific climate policies. Nevertheless, the addition of non-CO2 greenhouse gas and ozone precursor abatement options significantly reduces mitigation costs in the first half of the 21st century (by up to 40%) compared to the case where only CO2 abatement options are pursued. While the influences of aerosols are small by the end of the century, there is a significant interaction in the early 21st century between policies to reduce CO2 emissions and SO2 emissions, even in the presence of SO2-related pollution control policies. The attendant reduced aerosol cooling can more than offset the reduction in warming that accrues from reduced CO2. When non-CO2 gases are included in the policy, the net effect is that global-mean climate change to 2050 is practically unaffected by mitigation policy. [ABSTRACT FROM AUTHOR]