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Figure Average change in European glaciers
Located in Data and maps Maps and graphs
File The fourth assessment: Presentation of the report at the Belgrade conference
Subtitled movie of the speech hold by Executive Director of the EEA Jacqueline McGlade during the presentation of the 4th pan-European assessment at the UNECE 6th Мinisterial Conference "Environment for Europe", in Belgrade, 10th of October 2007.
Located in Environmental topics Archive: the Belgrade ministerial conference Videos and interviews
File Living with Climate change
Global warming is happening. Temperatures have already risen by 0.76 degrees since the industrial revolution and are projected to rise further by 1.8 - 4 degrees by the end of the century. The last time climate change happened at this pace was 125,000 years ago and led to a 4-6 metre sea level rise. Global warming at the upper end of the scale predicted by the Intergovernmental Panel on Climate Change would have catastrophic consequences for Europe. Up to 30% of plant, animal and bird species would be wiped out and the threat of natural disasters such as landslides, floods and mudslides would increase significantly.
Located in Environmental topics Climate change Multimedia
File Effects of climate change
In the past 100 years, the number of cold and frost days has decreased in most parts of Europe, whereas the number of days with temperatures above 25°C and the number of heatwaves have increased. The frequency of very wet days has significantly decreased in recent decades in many places in southern Europe, but increased in mid and northern Europe. Cold winters are projected to disappear almost entirely by 2080 and hot summers are projected to become much more frequent. This will have a continuing effect on mountain regions. For every 1°C increase in temperature, the snowline rises by 150 metres. And by 2050, three-quarters of today's glaciers in parts of the Alps are expected to have disappeared. Source: State of the Environment Report No 1/2005 "The European environment - State and outlook 2005" (published 29 Nov 2005)
Located in Environmental topics Climate change Multimedia
File PostScript document Rising snowline in the Alps
(This video has no audio.) It is estimated that, as global warming proceeds, regions currently receiving snowfall will increasingly receive precipitation in the form of rain. For every 1ºC increase in temperature, the snowline rises by about 150 metres. As a result, less snow will accumulate at low elevations. As a consequence, nearly half of all ski resorts in Switzerland, and even more in Germany, Austria and the Pyrenees, will face difficulties in attracting tourists and winter sport enthusiasts in the future. Source: EEA Report No 2/2004 "Impacts of Europe's changing climate" (published 18 Aug 2004)
Located in Environmental topics Climate change Multimedia
Figure Cumulative specific net mass balance of European glaciers
The figure shows the cumulative specific net mass balance (mm water equivalent) of European glaciers 1946–2010.
Located in Data and maps Maps and graphs
Article PostScript document Alps — The impacts of climate change in Europe today
Located in Signals — well-being and the environment Signals 2010
Article C source code Arctic — why should I care?
Located in Signals — well-being and the environment Signals 2010
Figure Cumulative specific net mass balance of selected glaciers from European glaciated regions, 1946–2008
Cumulative specific net mass balance of selected glaciers from European glaciated regions
Located in Data and maps Maps and graphs
Publication Understanding climate change — SOER 2010 thematic assessment
Average global air and ocean temperatures are rising, leading to the melting of snow and ice and rising global mean sea level. Ocean acidification results from higher CO2 concentrations. With unabated greenhouse gas emissions, climate change could lead to an increasing risk of irreversible shifts in the climate system with potentially serious consequences. Temperature rises of more than 1.5–2 °C above pre-industrial levels are likely to cause major societal and environmental disruptions in many regions. The atmospheric CO2 concentration needs to be stabilised at 350–400 parts per million (ppm) in order to have a 50 % chance of limiting global mean temperature increase to 2 °C above pre-industrial levels (according to the IPCC in 2007, and confirmed by later scientific insights).
Located in The European environment – state and outlook 2010 Thematic assessments
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