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Climate change, impacts and vulnerability in Europe ... - MemoFin.fr

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Changes <strong>in</strong> the climate systemSeveral studies have applied global climate modelsto estimate the warm<strong>in</strong>g associated with differentRCPs. These studies project an <strong>in</strong>crease <strong>in</strong> globalmean temperature by 2100, relative to pre<strong>in</strong>dustriallevels (1850–1900), of 1.5–2.3 °C for the lowest RCP(RCP2.6) to 4.5–5.8 °C for the highest RCP (RCP8.5)(Arora et al., 2011; Me<strong>in</strong>shausen et al., 2011; Meehlet al., 2012). The RCPs have been extended until 2300by the so-called extended concentration pathways(ECPs). Simulations us<strong>in</strong>g the ECPs suggest bestestimates for global mean temperature <strong>in</strong>crease by2300, relative to pre<strong>in</strong>dustrial levels, of 1.1 °C for theextension of RCP2.6 to 8.0 °C for the extension ofRCP8.5 (Me<strong>in</strong>shausen et al., 2011).<strong>Europe</strong>:The average temperature over <strong>Europe</strong> is projectedto cont<strong>in</strong>ue <strong>in</strong>creas<strong>in</strong>g throughout the 21st century.Accord<strong>in</strong>g to results <strong>fr</strong>om the ENSEMBLES project(van der L<strong>in</strong>den <strong>and</strong> Mitchell, 2009) the annualaverage l<strong>and</strong> temperature over <strong>Europe</strong> is projectedto <strong>in</strong>crease by more than global l<strong>and</strong> temperature.The annual temperature for <strong>Europe</strong> is projected to<strong>in</strong>crease by 1.0 °C to 2.5 °C (between periods2021–2050 <strong>and</strong> 1961–1990) <strong>and</strong> 2.5 °C to 4.0 °C(between periods 2071–2100 <strong>and</strong> 1961–1990).The warm<strong>in</strong>g is projected to be the greatest <strong>in</strong>north‐eastern <strong>Europe</strong> <strong>and</strong> Sc<strong>and</strong><strong>in</strong>avia <strong>in</strong> w<strong>in</strong>ter <strong>and</strong>over southern <strong>Europe</strong> <strong>in</strong> summer (Map 2.2). Note thatmaps about trends <strong>and</strong> projections are not directlycomparable because complex processes, variability<strong>and</strong> feedbacks mean that past trends cannot beassumed to cont<strong>in</strong>ue at the same rate <strong>in</strong>to the future.Map 2.2Projected <strong>change</strong>s <strong>in</strong> annual, summer <strong>and</strong> w<strong>in</strong>ter temperature across <strong>Europe</strong>Annual, 2021–2050Summer, 2021–2050W<strong>in</strong>ter, 2021–205050°50°50°40°40°40°0°10°20°30°40°0°10°20°30°40°0°10°20°30°40°Annual, 2071–2100Summer, 2071–2100W<strong>in</strong>ter, 2071–210050°50°50°40°40°40°0°10°20°30°40°0°10°20°30°40°0°10°20°30°40°Projected <strong>change</strong>s <strong>in</strong> annual, summer <strong>and</strong> w<strong>in</strong>ter temperature 2021–2050 (top) <strong>and</strong> 2071–2100 (bottom)0.5 1 1.5 2 2.5 3 3.5 4 4.5°C No dataNote:Projected <strong>change</strong>s <strong>in</strong> annual (left), summer (JJA; centre), <strong>and</strong> w<strong>in</strong>ter (DJF; right) near-surface air temperature (°C) for theperiod 2021–2050 (above) <strong>and</strong> 2071–2100 (below), compared to 1961–1990. Projections are based on the ENSEMBLESproject. They have been obta<strong>in</strong>ed <strong>fr</strong>om different regional climate models (RCMs) perform<strong>in</strong>g at 25 km spatial resolution withboundary conditions <strong>fr</strong>om five global climate models (GCMs), all us<strong>in</strong>g the IPCC SRES A1B emission scenario.Source: van der L<strong>in</strong>den <strong>and</strong> Mitchell, 2009.<strong>Climate</strong> <strong>change</strong>, <strong>impacts</strong> <strong>and</strong> <strong>vulnerability</strong> <strong>in</strong> <strong>Europe</strong> 201261

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