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Trend in absolute sea level across Europe based on satellite measurements (1992–2011)
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Based on satellite data; trends in mm/year, inverted barometer included, seasonal signal removed
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Data and maps
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Maps and graphs
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National Renewable Energy Action Plan (NREAP) data from Member States
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A compiled dataset on renewable energy trajectories extracted from the submissions of the Member States to the European Commission, and an accompanying document which summarises the main points of the data.
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Maps and graphs
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Big potential of cutting greenhouse gases from waste
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There is a big potential to cut greenhouse gases (GHGs) from municipal solid waste management, according to a new report from the European Environment Agency (EEA). The report, 'Waste opportunities – Past and future climate benefits from better municipal waste management in Europe', covers the EU-27 (excluding Cyprus), Norway and Switzerland. It estimates that these countries could make GHG savings of up to 78 million tonnes carbon dioxide equivalent (CO2-e) by 2020, or 1.53 % of Europe's emissions in 2008.
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News
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The fourth assessment: Presentation of the report at the Belgrade conference
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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.
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Environmental topics
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…
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Archive: the Belgrade ministerial conference
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Videos and interviews
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Arctic sea ice (CLIM 010) - Assessment published Sep 2008
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The extent of the sea ice in the Arctic has declined at an accelerating rate, especially in summer. The record low ice cover in September 2007 was roughly half the size of the normal minimum extent in the 1950s. The summer ice is projected to continue to shrink and may even disappear at the height of the summer melt season in the coming decades. There will still be substantial ice in winter. Reduced polar ice will speed up global warming and is expected to affect ocean circulation and weather patterns. Species specialised for life in the ice are threatened. Less ice will ease access to the Arctic's resources. Oil and gas exploration, shipping, tourism and fisheries will offer new economic opportunities, but also increase pressures and risks to the Arctic environment.
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Arctic sea ice
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CC_F03: GHG emissions - outlook from IIASA (Outlook 031) - Assessment published Jun 2007
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The RAINS* model provides information about the projections for the methane emissions. For the "current legislation" scenario a continued increase of global anthropogenic CH4 emissions is expected, leading to 35 percent increase in 2030 as compared to 2000. CH4 emissions from all sectors are expected to grow due to increased economic activities and absence of wide-spread emission control measures. In Western Europe and Newly Independent states overall CH4 emissions will only slightly increase. If all maximum technically feasible reductions (MFR scenario) were applied to the full extent, global CH4 emissions would stabilize up to 2030, though at considerable costs. Under the MFR scenario CH4 emissions in Western Europe and Newly Independent states would be able to decrease on 31% and 16% relatively.
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CC_F03: GHG emissions - outlook from IIASA
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Coastal areas (CLIM 041) - Assessment published Sep 2008
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Coastal flooding can lead to important losses. By 2100, the population in the main coastal European cities exposed to sea-level rise and associated impacts on coastal systems is expected to be about 4 million and the exposed assets more than EUR 2 trillion (without adaptation). Future projections of sea-level rise and associated impacts on coastal systems show potentially large increases in the risk of coastal flooding. These could have significant economic costs (without adaptation), with recent estimates in the range of 12 to 18 billion EUR/year for Europe in 2080 under the IPCC SRES A2 scenario. The same estimates indicate that adaptation could significantly reduce this risk to around EUR 1 billion.
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Coastal areas
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Crop-yield variability (CLIM 032) - Assessment published Sep 2008
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Climate and its variability are largely responsible for variations in crop suitability and productivity in Europe. Since the beginning of the 21st century, the variability of crop yields has increased as a consequence of extreme climatic events, e.g. the summer heat of 2003 and the spring drought of 2007. As a consequence of climatic change, such events are projected to increase in frequency and magnitude, and crop yields to become more variable. Changes in farming practices and land management can act as risk-mitigating measures.
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Crop-yield variability
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Final energy consumption - outlook from IEA (Outlook 011) - Assessment published Jun 2007
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Aggregate global demand in final-use sectors is projected to grow by 1.4% per year from 2006 to 2030 - slightly slower than primary energy demand. The fastest growth is projected in non-OECD countries, while OECD Europe's growth in final energy consumption is expected to be the lowest pace. Industry demand increases everywhere, but fastest in the Middle East, India and China. The rate of growth in global transport energy demand slows considerably over the Outlook period. In 2030, disparities in per capita energy consumption among regions are projected to remain stark. Russia and OECD countries are expected continue having significantly higher levels of final energy consumption per capita than in other world regions.
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Final energy consumption - outlook from IEA
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Glaciers (CLIM 007) - Assessment published Sep 2008
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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.
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Glaciers