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Aviation and the Global Atmosphere

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<strong>Aviation</strong> <strong>and</strong> <strong>the</strong> <strong>Global</strong> <strong>Atmosphere</strong><br />

The RF uncertainties from different perturbations have been determined by different methods; potential errors in individual components may not be independent of one<br />

ano<strong>the</strong>r, <strong>and</strong> <strong>the</strong> error bars may not represent Gaussian statistics. The uncertainty ranges for <strong>the</strong> totals in Figures 6-14b <strong>and</strong> 6-15b do represent a 2/3 probability range<br />

as for <strong>the</strong> individual components. The uncertainty estimate for <strong>the</strong> total radiative forcing (without additional cirrus) is calculated directly from <strong>the</strong> individual components<br />

as <strong>the</strong> square root of <strong>the</strong> sums of <strong>the</strong> squares of <strong>the</strong> upper <strong>and</strong> lower ranges. There is a fur<strong>the</strong>r issue on confidence levels that is not quantified here-namely, <strong>the</strong><br />

accuracy of representing <strong>the</strong> climate perturbation by <strong>the</strong> sum of RF values that are global means.<br />

Overall, addition of <strong>the</strong> best values for RF provides a single best estimate for <strong>the</strong> total. The uncertainty ranges for individual impacts can be used to assess whe<strong>the</strong>r<br />

<strong>the</strong>y are potentially major or trivial components <strong>and</strong> to make a subjective judgment of confidence in <strong>the</strong> summed RF.<br />

Table of contents | Previous page | Next page<br />

O<strong>the</strong>r reports in this collection<br />

http://www.ipcc.ch/ipccreports/sres/aviation/084.htm (2 von 2)08.05.2008 02:43:13<br />

IPCC Homepage

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