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

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<strong>Climate</strong> <strong>impacts</strong> on environmental systemsperiod <strong>and</strong> three future time periods based on thehydrological model LISFLOOD <strong>and</strong> an ensemble of12 climate models. Blue rivers <strong>in</strong>dicate an <strong>in</strong>crease<strong>in</strong> flood level <strong>and</strong> red rivers a decrease. While theensemble mean presented <strong>in</strong> Map 3.8 provides thebest assessment of all model simulations together,<strong>in</strong>dividual simulations can show importantdifferences <strong>fr</strong>om the ensemble mean for <strong>in</strong>dividualcatchments, partly due to significant decadal-scale<strong>in</strong>ternal variability <strong>in</strong> the simulated climate (Feyenet al., 2011). A decrease <strong>in</strong> 1-<strong>in</strong>-a-century floods isprojected <strong>in</strong> large parts of north-eastern <strong>Europe</strong> dueto a reduction <strong>in</strong> snow accumulation <strong>and</strong> hence meltassociatedfloods under milder w<strong>in</strong>ter temperatures(Dankers <strong>and</strong> Feyen, 2009). This projection isconsistent with other studies on snow-dom<strong>in</strong>atedregions, <strong>in</strong>clud<strong>in</strong>g parts of F<strong>in</strong>l<strong>and</strong> (Veijala<strong>in</strong>en et al.,2010), the Alps <strong>and</strong> Carpathian Mounta<strong>in</strong>s (EEA,2009b). Flash floods <strong>and</strong> pluvial floods, which aretriggered by local <strong>in</strong>tense precipitation events, arelikely to become more <strong>fr</strong>equent throughout <strong>Europe</strong>(Christensen <strong>and</strong> Christensen, 2002; Kundzewiczet al., 2006).3.3.4 River flow droughtRelevanceLack of water has severe consequences for <strong>Europe</strong>'scitizens <strong>and</strong> most economic sectors, <strong>in</strong>clud<strong>in</strong>gagriculture, energy production <strong>and</strong> <strong>in</strong>dustry. An<strong>in</strong>tense drought throughout the Iberian Pen<strong>in</strong>suladur<strong>in</strong>g 2004–2005, for example, led to a 40 %decl<strong>in</strong>e <strong>in</strong> cereal production (García-Herrera et al.,2007), whilst low ra<strong>in</strong>fall <strong>in</strong> 2006 led to a 30 %fall <strong>in</strong> agricultural production <strong>in</strong> Lithuania, withan estimated loss of EUR 200 million (<strong>Europe</strong>anCommission, 2007). In Slovenia, direct lossesattributable to drought <strong>in</strong> 2003 are estimated to bearound EUR 100 million (Sušnik <strong>and</strong> Kurnik, 2005).Furthermore, lack of water detrimentally <strong>impacts</strong><strong>fr</strong>eshwater ecosystems <strong>in</strong>clud<strong>in</strong>g vegetation, fish,<strong>in</strong>vertebrates <strong>and</strong> riparian bird life (EEA, 2009a).Dim<strong>in</strong>ished flow also strongly <strong>impacts</strong> water qualityby reduc<strong>in</strong>g the ability of a river to dilute pollutants.Electricity production has already been significantlyreduced <strong>in</strong> various locations <strong>in</strong> <strong>Europe</strong> dur<strong>in</strong>g verywarm summers due to limitations of cool<strong>in</strong>g watersupply <strong>fr</strong>om rivers. Dry periods can also seriouslyimpact the production of hydropower (Lehner et al.,2005), for example <strong>in</strong> the case of Catalunia where the2003–2007 drought caused a hydropower reductionof over 40 % (Generalitat de Catalunya, 2010).Past trendsOver the past 40 years, <strong>Europe</strong> has been affected bya number of major droughts, most notably <strong>in</strong> 1976,1989, 1991, <strong>and</strong> more recently (see Map 3.9), theprolonged drought over large parts of the cont<strong>in</strong>entassociated with the 2003 summer heat wave <strong>and</strong>the 2005 drought <strong>in</strong> the Iberian Pen<strong>in</strong>sula (see alsoeffects on Energy production <strong>in</strong> Section 4.5).However, there is no evidence that river flowdroughts have become more severe or <strong>fr</strong>equent over<strong>Europe</strong> <strong>in</strong> general <strong>in</strong> recent decades (Hisdal et al.,2001; Stahl et al., 2008), nor is there conclusive proofof a general <strong>in</strong>crease <strong>in</strong> summer dryness (based onthe Palmer Drought Severity Index) <strong>in</strong> <strong>Europe</strong> overthe past 50 years due to reduced summer moistureavailability (van der Schrier et al., 2006). Severalstations <strong>in</strong> <strong>Europe</strong> have shown trends towards lesssevere low stream flows over the 20th century butthis is primarily attributed to an <strong>in</strong>creas<strong>in</strong>g numberof reservoirs becom<strong>in</strong>g operational dur<strong>in</strong>g thisperiod (Svensson et al., 2005).Whilst public water supplies often have priorityover other uses dur<strong>in</strong>g droughts, restrictionson use can arise, together with a significant costassociated with emergency water supplies. In2008, Cyprus suffered its fourth consecutive yearof low ra<strong>in</strong>fall <strong>and</strong> the drought situation reacheda critical level <strong>in</strong> the summer months. To ease thecrisis, water was shipped <strong>in</strong> <strong>fr</strong>om Greece us<strong>in</strong>gKey messages: 3.3.4 River flow drought• <strong>Europe</strong> has been affected by several major droughts <strong>in</strong> recent decades, such as the catastrophicdrought associated with the 2003 summer heat wave <strong>in</strong> central parts of the cont<strong>in</strong>ent <strong>and</strong> the 2005drought <strong>in</strong> the Iberian Pen<strong>in</strong>sula.• Severity <strong>and</strong> <strong>fr</strong>equency of droughts appear to have <strong>in</strong>creased <strong>in</strong> parts of <strong>Europe</strong>, <strong>in</strong> particular <strong>in</strong>southern <strong>Europe</strong>.• Regions most prone to an <strong>in</strong>crease <strong>in</strong> drought hazard are southern <strong>and</strong> south-eastern <strong>Europe</strong>, butm<strong>in</strong>imum river flows are also projected to decrease significantly <strong>in</strong> many other parts of the cont<strong>in</strong>ent,especially <strong>in</strong> summer.120 <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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