15.11.2014 Views

World Energy Outlook 2007

World Energy Outlook 2007

World Energy Outlook 2007

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Box 5.3: IPCC Fourth Assessment Report<br />

The <strong>World</strong> Meteorological Organisation (WMO) and the United Nations<br />

Environment Programme (UNEP) established the Intergovernmental Panel<br />

on Climate Change (IPCC) in 1988 to assess scientific, technical and socioeconomic<br />

information relevant for the understanding of climate change, its<br />

potential impacts and options for adaptation and mitigation. The IPCC has<br />

three working groups (WGs) which assess knowledge of the climate system<br />

(WG I), the impact of the adaptation to climate change (WG II) and the<br />

mitigation of climate change (WG III), plus a Task Force on national<br />

greenhouse-gas inventories. The assessments are performed by scientists<br />

nominated by governments and scientific organisations. They are managed<br />

by an elected bureau and are supported by the IPCC Secretariat and the<br />

Technical Support Units of the working groups. The IPCC meets in<br />

plenary session about once a year to approve the work programme and the<br />

assessment reports,.<br />

A main activity of the IPCC is to provide at regular intervals an assessment<br />

of the state of knowledge about climate change. It recently finalised and<br />

released the three working group reports that will make up its Fourth<br />

Assessment Report, providing a comprehensive and up-to-date appraisal of<br />

the current state of knowledge on climate change. A synthesis report is due<br />

to be released in November <strong>2007</strong>.<br />

5<br />

The global atmospheric concentration of CO 2<br />

has increased from a<br />

pre-industrial level of about 280 parts per million to 379 ppm in 2005.<br />

This level exceeds by far the natural range over the last 650 000 years<br />

(180 to 300 ppm) as determined from ice cores. It is estimated that, were<br />

CO 2<br />

concentrations to rise to 400 to 440 ppm and stabilise at that level, the<br />

eventual rise in global average temperature would amount to around 2.4° to<br />

2.8°C (IPCC, <strong>2007</strong>). In order to stabilise the concentration of CO 2<br />

in the<br />

atmosphere, emissions would need to peak and decline thereafter. The lower<br />

the target stabilisation level, the more quickly this peak and decline would<br />

need to occur. For this reason, mitigation efforts over the next two to three<br />

decades will affect our ability to achieve lower stabilisation levels. Based on<br />

current understanding of climate-carbon cycle feedback, the IPCC<br />

concludes that, in order to stabilise CO 2<br />

-equivalent 4 concentrations at 445-<br />

490 ppm, CO 2<br />

emissions would need to peak by 2015 at the latest and fall<br />

to between 50% and 85% below 2000 levels by 2050. A later peak and less<br />

sharp reductions in emissions would lead to higher concentrations and<br />

bigger increases in temperature (Table 5.4).<br />

4. All greenhouse gases expressed in CO 2<br />

-equivalent terms (adjusted for differences in radiative<br />

forcing).<br />

Chapter 5 - Global Environmental Repercussions 205

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!