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World Energy Outlook 2007

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Figure 5.11: Change in Carbon Intensity by Region and Scenario, 2005-2030<br />

Transition<br />

economies<br />

OECD<br />

Other developing<br />

countries<br />

India<br />

China<br />

–70% –60% –50% –40% –30% –20% –10% 0%<br />

Reference Scenario<br />

Alternative Policy Scenario<br />

High Growth Scenario<br />

Implications for Climate Change<br />

There now exists a major body of scientific evidence that rising greenhouse-gas<br />

concentrations in the atmosphere resulting from fossil-energy combustion and<br />

other human activities are contributing to rising global temperatures and to<br />

changes in climate patterns. Today, the link between greenhouse-gas emissions<br />

and climate change is accepted by the overwhelming majority of scientists, even<br />

if the magnitude and nature of the changes that will follow from a given rise in<br />

emissions are still very uncertain. The primary source of the increased<br />

atmospheric concentration of greenhouse gases since the pre-industrial period<br />

has been the burning of fossil fuels, with land-use change providing another<br />

significant, but smaller, contribution.<br />

The latest assessment of the Intergovernmental Panel on Climate Change (IPCC)<br />

concludes that most of the observed increase in global average temperatures since<br />

the mid-20th century is very likely to be due to the observed increase in<br />

anthropogenic greenhouse-gas concentrations, notably CO 2<br />

(Box 5.3). Continued<br />

greenhouse-gas emissions at or above current rates would drive atmospheric<br />

concentrations even higher, causing further warming and inducing many changes<br />

in the global climate system during the 21st century that would very likely be<br />

larger than those observed during the 20th century (IPCC, <strong>2007</strong>). These<br />

conclusions were somewhat stronger than those of the previous assessment,<br />

reflecting important advances in the knowledge and understanding of climate<br />

change. Even if concentrations are stabilised, some anthropogenic warming and<br />

rises in sea levels are expected to continue for centuries, due to the time-scales<br />

associated with climate processes and feedbacks.<br />

204 <strong>World</strong> <strong>Energy</strong> <strong>Outlook</strong> <strong>2007</strong> - GLOBAL ENERGY PROSPECTS: IMPACT OF DEVELOPMENTS IN CHINA & INDIA

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