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The figure shows the past and projected change in global surface temperatures. If global greenhouse gas emissions would not be reduced, the 2°C target will be exceeded towards the middle of the 21st century. The horizontal 2°C target line takes into account warming of about 0.6 °C from pre-industrial to 1990. “Likely” ranges in average 2090-2099 warming for all six IPCC scenarios are shown on the right
These graphs show the trends in the use of material resources in EU-15 and EU-12 and municipal waste generation in EU‑27 compared with GDP and population.
This graph shows the intensity of forestry — net annual increment in growing stock and annual fellings of forest available for wood supply — 32 EEA member countries, 1990–2005.
Temperature increase (above 1990 level) at which the various events could occur and an estimate of their impact. The impact scale has subjective qualifications (‘minor’, ‘notable’, ‘major’ and ‘devastating’), which were assigned on the basis of the geographical scale (from ‘regional’ to ‘continental’ and ‘global’) and the character of the damages (‘light’, ‘moderate’, ‘heavy’ or ‘extreme’). The level of scientific understanding, as well as the understanding of possible impacts for most of these events is low. The shapes and sizes of the ovals do not represent uncertainties in impact and temperature onset of eventualities and these uncertainties may be significant.
The EEA welcomes the publication today of UNEP's report 'Pathways to a green economy'. It represents a valuable contribution to the current debate on moving the world to a sustainable path in the 21st century.
The ‘pH’ is a measure of acidity – the lower the number the more acidic the ocean becomes. On a geological timescale, ocean pH has been relatively stable. Recently, oceans have been acidifying fast and this is projected to continue at a rate unprecedented for millions of years.
Note: The maps on the left show the area of the Greenland ice sheet with at least one day of surface melting in summer. The diagram on the left shows the cumulated melt area, which is defined as the annual total sum of every daily ice sheet melt area. For example, if a particular area is melting on 20 days in a given year, it is counted 20 times.
Cumulative specific net mass balance of selected glaciers from European glaciated regions
Present and projected water limitation of crop primary production in Europe under rain-fed conditions
For references, please go to https://www.eea.europa.eu/soer/2010/advanced-search or scan the QR code.
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