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By Nadia Shalaby, Yitzchak Gottlieb, Mike Wawrzoniak, Larry Peterson (auth.), James Sterbenz, Osamu Takada, Christian Tschudin, Bernhard Plattner (eds.)

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Additional resources for Active Networks: IFIP-TC6 4th International Working Conference, IWAN 2002 Zurich, Switzerland, December 4–6, 2002 Proceedings

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CCIPs try to go several steps further by quantifying specific climate perturbations that are more directly related to different kinds of climate-change impacts. The functions used to calculate CCIPs still retain simplicity and transparency. The use of CCIPs instead of 100-year GWPs would reduce the shortterm emphasis on CH4 as CH4 emitted in 2010 will have disappeared from the atmosphere by the time the most damaging temperatures or rates of warming will be reached. g. Shine et al 2007). However, even CH4 contributes to cumulative-warming impacts.

These calculations would need to be repeated every few years with new scientific understanding and newer emission projections to provide 14 Climate Policy: International Perspectives on Greenhouse Gases updated guidance of the importance of different GHG over the next 100year period. 2 CALCULATING RADIATIVE FORCING AND TEMPERATURE CHANGES The calculations of radiative forcing and temperature followed the approach of Kirschbaum et al (2013), including the carbon cycle based on the Bern model and radiative forcing calculations provided by the IPCC.

A 365 1903–14 Climate-Change Impact Potentials as an Alternative to Global Warming Potentials 31 42. Shine K P, Fuglestvedt J S, Hailemariam K and Stuber N 2005 Alternatives to the global warming potential for comparing climate impacts of emissions of greenhouse gases Clim. Change 68 281–302 43. Smith S M, Lowe J A, Bowerman N H A, Gohar L K, Huntingford C and Allen M R 2012 Equivalence of greenhouse-gas emissions for peak temperature limits Nature Clim. Change 2 535–8 44. hmtreasury. cfm) 45. Sterner T and Persson U M 2008 An even sterner review: introducing relative prices into the discounting debate Rev.

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