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Summary for Policymakers<br />

before 2100, in which case they are about as likely as not to achieve that goal. In these 500 ppm C0 2-eq scenarios, global 2050<br />

emissions levels are 25 to 55% lower than in 2010. Scenarios with higher emissions in 2050 are characterized by a greater<br />

reliance on Carbon Dioxide Removal (CDR) technologies beyond mid-century (and vice versa). Trajectories that are likely to<br />

limit warming to 3°C relative to pre-industrial levels reduce emissions less rapidly than those limiting warming to 2 0 C. A limited<br />

number of studies provide scenarios that are more likely than notXo limit warming to 1.5 0 C by 2100; these scenarios are<br />

characterized by concentrations below 430 ppm C0 2-eq by 2100 and 2050 emission reduction between 70% and 95% below<br />

2010. For a comprehensive overview of the characteristics of emissions scenarios, their C0 2-equivalent concentrations and<br />

their likelihood to keep warming to below a range of temperature levels, see Figure SPM.11 and Table SPM.I. {3.4}<br />

GHG emission pathways 2000-2100: All AR5 scenarios<br />

120<br />

[ 530-580 ppm COj-eq<br />

80<br />

• 480-530 ppm COj-eq<br />

• 430-480 ppm C03-eq<br />

- - Full AR5 database range<br />

(b)<br />

100<br />

Associated upscaling of low-carbon energy supply<br />

80<br />

60<br />

40<br />

20<br />

2010<br />

2030 2050 2100 2030 2050 2100 2030 2050 2100 2030 2050 2100<br />

Figure SPM.11 | Global greenhouse gas emissions (gigatonne of C0 3-equivalent per year, GtC0 2-eq/yr) in baseline and mitigation scenarios for different<br />

long-term concentration levels (a) and associated upscaling requirements of low-carbon energy (% of primary energy) for 2030,2050 and 2100 compared<br />

to 2010 levels in mitigation scenarios (b). {Figure 3.2]<br />

App. 469<br />

21

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