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

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Changes <strong>in</strong> the climate systemMap 2.4Projections of extreme high temperatures1961–1990 2021–2050 2071–21000 1500 km 0 1500 km 0 1500 kmNumber of comb<strong>in</strong>ed tropical nights (> 20 °C) <strong>and</strong> hot days (> 35 °C)No data0 2 6 10 14 18 22 26 30 34 38 42 46 50Outside coverageNote:Extreme high temperatures are represented by the comb<strong>in</strong>ed number of hot summer (June–August) days (TMAX > 35 °C)<strong>and</strong> tropical nights (TMIN > 20 °C). All projections are the average of six regional climate model (RCM) simulations of theEU ENSEMBLES project us<strong>in</strong>g the IPCC SRES A1B emission scenario for the periods 1961–1990, 2021–2050 <strong>and</strong> 2071–2100.Source: Fischer <strong>and</strong> Schär, 2010. © Nature Publish<strong>in</strong>g Group. Repr<strong>in</strong>ted with permission.2.2.4 Mean precipitationRelevancePrecipitation plays a vital role <strong>in</strong> allhuman‐environment systems <strong>and</strong> sectors, <strong>in</strong>clud<strong>in</strong>gagriculture, water supply, energy production,tourism <strong>and</strong> natural ecosystems. Daily precipitationtotals are st<strong>and</strong>ard meteorological measures thathave been recorded systematically s<strong>in</strong>ce the 1860s.However, despite longevity of the precipitationrecord <strong>in</strong> certa<strong>in</strong> areas, the high spatial <strong>and</strong>temporal variability of precipitation means thatthe climate <strong>change</strong> signal cannot be detected withcerta<strong>in</strong>ty <strong>in</strong> all <strong>Europe</strong>an regions. Difficulties fordetect<strong>in</strong>g a significant trend can arise <strong>fr</strong>om thesmall sampl<strong>in</strong>g area of ra<strong>in</strong> gauges, calibrationerrors <strong>in</strong> <strong>in</strong>strumentation, erroneous measurementsdur<strong>in</strong>g weather conditions such as snow or gales,<strong>and</strong> <strong>fr</strong>om limited sampl<strong>in</strong>g of the spatial variabilityof precipitation, such as <strong>in</strong> mounta<strong>in</strong>ous areas.Therefore, observed <strong>and</strong> projected precipitation<strong>change</strong>s should always be considered <strong>in</strong> the contextof <strong>in</strong>terannual variability <strong>and</strong> the measurement ormodell<strong>in</strong>g uncerta<strong>in</strong>ty.Key messages: 2.2.4 Mean precipitation• Annual precipitation trends s<strong>in</strong>ce 1950 show an <strong>in</strong>crease by up to 70 mm per decade <strong>in</strong> north-eastern<strong>and</strong> north-western <strong>Europe</strong> <strong>and</strong> a decrease by up to 70 mm <strong>in</strong> some parts of southern <strong>Europe</strong>.• Seasonal precipitation trends show an <strong>in</strong>crease <strong>in</strong> w<strong>in</strong>ter precipitation <strong>in</strong> northern <strong>Europe</strong> <strong>and</strong> adecrease <strong>in</strong> southern <strong>Europe</strong>, albeit with large <strong>in</strong>terannual variations.• There is a robust signal <strong>fr</strong>om regional simulations across many parts of central <strong>and</strong> western <strong>Europe</strong>across all seasons. However, many parts of <strong>Europe</strong>, such as eastern <strong>and</strong> southern <strong>Europe</strong>, lack modelconsensus on the direction of <strong>change</strong>.<strong>Climate</strong> <strong>change</strong>, <strong>impacts</strong> <strong>and</strong> <strong>vulnerability</strong> <strong>in</strong> <strong>Europe</strong> 201265

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