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EEAFigure Average change in European glaciers
Located in Data and maps Maps and graphs
File Climate change — time to act
Climate change is a real and current threat. To avoid major irreversible impacts on society and ecosystems, we must act now.
Located in Multimedia centre
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
Indicator Assessment Glaciers (CLIM 007) - Assessment published Sep 2008
The vast majority of glaciers in the European glacial regions are in retreat. Since 1850, glaciers in the European Alps have lost approximately two thirds of their volume, with clear acceleration since the 1980s. Glacier retreat is projected to continue. A 3 o C increase in average summer air temperature could reduce the existing glacier cover of the European Alps by some 80 %. With continuing climate change nearly all the smaller glaciers and one third of the overall glacier area in Norway are projected to disappear by 2100. Glacier retreat has serious consequences for river flow. It affects freshwater supply, river navigation, irrigation and power generation. It could cause natural hazards and damage to infrastructure.
Located in Data and maps Indicators Glaciers
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 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
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
Publication Adapting to climate change - SOER 2010 thematic assessment
Climate change is happening and will continue to have far-reaching consequences for human and natural systems. Impacts and vulnerabilities differ considerably across regions, territories and economic sectors in Europe. Strategies to adapt to climate change are necessary to manage impacts even if global temperature stays below a 2 °C increase above the pre-industrial level. The EU adaptation framework aims at developing a comprehensive strategy by 2013, to be supported by a clearinghouse for sharing and maintaining information on climate change impacts, vulnerability and adaptation.
Located in The European environment – state and outlook 2010 Thematic assessments
SOER Message Understanding climate change — key message 5
The vast majority of glaciers in Europe are in retreat. Glaciers in the Alps lost about two-thirds of their volume between 1850 and 2009. The glacierised area in the Alps is projected to decrease to about one-third of the present area for a further rise in Alpine summer temperature of 2 °C.
Located in The European environment – state and outlook 2010 Understanding climate change — SOER 2010 thematic assessment Key messages
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