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

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Changes <strong>in</strong> the climate systemPast trendsAnnual precipitation records averaged across<strong>Europe</strong> show no significant <strong>change</strong>s s<strong>in</strong>ce 1950accord<strong>in</strong>g to the E-OBS dataset (Haylock et al., 2008),based on the <strong>Europe</strong>an <strong>Climate</strong> Assessment dataset(Klok <strong>and</strong> Kle<strong>in</strong> Tank, 2009). At the sub-cont<strong>in</strong>entalscale, the trend <strong>in</strong> precipitation is most significant<strong>in</strong> north-eastern <strong>and</strong> south-western <strong>Europe</strong>. Themajority of Sc<strong>and</strong><strong>in</strong>avia <strong>and</strong> the Baltic States haveobserved an <strong>in</strong>crease <strong>in</strong> annual precipitation ofgreater than 14 mm per decade, with an <strong>in</strong>creaseof up to 70 mm per decade <strong>in</strong> western Norway. Incontrast, annual precipitation has decreased <strong>in</strong> theIberian Pen<strong>in</strong>sula, <strong>in</strong> particular <strong>in</strong> north-westernSpa<strong>in</strong> <strong>and</strong> <strong>in</strong> northern Portugal (Map 2.5). Whilethere is some evidence l<strong>in</strong>k<strong>in</strong>g l<strong>and</strong> use, <strong>in</strong> particularforest cover, to local <strong>and</strong> regional precipitationpatterns (Millán, 2008), it is not clear if the relativelym<strong>in</strong>or l<strong>and</strong>-use <strong>change</strong>s s<strong>in</strong>ce 1950 have <strong>in</strong>fluencedthe observed precipitation trends.ProjectionsSeasonal mean precipitation values <strong>and</strong> <strong>in</strong>ter-annualvariability is better reproduced by an ensembleof RCMs than by any s<strong>in</strong>gle RCM (Beniston et al.,2007; Tapiador, 2010). Recent work, build<strong>in</strong>g onthe two EU-funded research projects PRUDENCE(Christensen et al., 2002) <strong>and</strong> ENSEMBLES (van derL<strong>in</strong>den <strong>and</strong> Mitchell, 2009) has shown that RCMshave a reasonably strong consensus across <strong>Europe</strong><strong>in</strong> predict<strong>in</strong>g <strong>change</strong>s <strong>in</strong> seasonal average ra<strong>in</strong>fall(Tapiador, 2010). These projections <strong>in</strong>dicate a general<strong>in</strong>crease <strong>in</strong> annual precipitation <strong>in</strong> northern <strong>Europe</strong><strong>and</strong> a decrease <strong>in</strong> southern <strong>Europe</strong>. The <strong>change</strong> <strong>in</strong>annual mean between 1961–1990 <strong>and</strong> 2071–2100accord<strong>in</strong>g to the ENSEMBLES project (van derL<strong>in</strong>den <strong>and</strong> Mitchell, 2009) varies between 10% <strong>and</strong>20 % <strong>in</strong> northern <strong>Europe</strong> <strong>and</strong> between – 5 to – 20 %<strong>in</strong> southern <strong>Europe</strong> <strong>and</strong> the Mediterranean (Map 2.6left). Projections for summer precipitation showa decrease over southern, central <strong>and</strong> northwest<strong>Europe</strong>, which can reach of up to 60 % <strong>in</strong> parts ofsouthern <strong>Europe</strong>. Precipitation is projected to rema<strong>in</strong>constant or to <strong>in</strong>crease slightly <strong>in</strong> northeast <strong>Europe</strong>(van der L<strong>in</strong>den <strong>and</strong> Mitchell, 2009; Tapiador, 2010)(Map 2.6 right).Map 2.570N60N50N40N30N1 2001 000800600Note:Total precipitationDrier– 87.5– 7015W 0 15E 30E– 52.5– 35PRCPTOT (mm)Trends <strong>in</strong> annual precipitationacross <strong>Europe</strong> (1960–2012)Change <strong>in</strong> annual precipitation (PRCPTOT, mm/decade)– 17.5017.5Trend: – 35.99 mm per decade (– 59.30 to – 10.14)Trend: 30.10 mm per decade (12.60 to 46.56)3552.570Wetter87.51955 1965 1975 1985 1995 2005 2015The trends are calculated us<strong>in</strong>g a median of pairwiseslopes algorithm. Black dots represent high confidence<strong>in</strong> the sign of the long-term trend <strong>in</strong> the box (if the5th to 95th percentile slopes are of the same sign).Boxes which have a thick outl<strong>in</strong>e conta<strong>in</strong> at leastthree stations. Area averaged annual time series ofpercentage <strong>change</strong>s <strong>and</strong> trend l<strong>in</strong>es are shown beloweach map for one area <strong>in</strong> northern <strong>Europe</strong> (bluel<strong>in</strong>e, 5.6 to 16.9 °E <strong>and</strong> 56.2 to 66.2 °N) <strong>and</strong> one <strong>in</strong>south‐western <strong>Europe</strong> (red l<strong>in</strong>e, 350.6 to 1.9 °E <strong>and</strong>36.2 to 43.7 °N).Source: HadEX dataset, updated with data <strong>fr</strong>om the ECA&Ddataset.66 <strong>Climate</strong> <strong>change</strong>, <strong>impacts</strong> <strong>and</strong> <strong>vulnerability</strong> <strong>in</strong> <strong>Europe</strong> 2012

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