Climate change, impacts and vulnerability in Europe ... - MemoFin.fr
Climate change, impacts and vulnerability in Europe ... - MemoFin.fr Climate change, impacts and vulnerability in Europe ... - MemoFin.fr
Changes in the climate systemMap 2.8Projected changes in 20-year maximum precipitation in summer and winterSummerWinterProjected changes in 20-year maximum precipitation in summer and winter(%)– 40 – 20 0 20 40Note: Projected changes in 20-year maximum daily precipitation in summer (left) and winter (right) from 1961–1990 to 2071–2100based on the ensemble mean using a regional climate model (RCM) nested in 6 general circulation model (GCMs). Changesthat approximately lie outside of ± 10 % for the ensemble average are significant at the 10 % significance level.Source: Nikulin et al., 2011.2.2.6 StormsRelevanceStorms are atmospheric disturbances that aredefined by strong sustained wind. In many cases,they are accompanied by heavy precipitation (rain,hail or snow) and lightning. In Europe, storms canrange from relatively small and localised eventsto large features covering a substantial part of thecontinent. They typically develop from extra-tropicalcyclones which are low-pressure weather systemsthat occur between 30 and 80 °N and capture theirenergy from the temperature contrast between thesub-tropical and polar air masses that meet in theAtlantic Ocean. These extra-tropical cyclones areKey messages: 2.2.6 Storms• Storm location, frequency and intensity have shown considerable variability across Europe over the pastcentury, making it difficult to identify clear trends. A recent reanalysis suggests that storminess hasincreased over the past century in northern and north-western Europe but this finding is not yet robust.• Climate change projections for storms in the North Atlantic and Europe region show no clear consensusin either the direction of movement or the intensity of storm activity. However, a recent study involving20 climate models projects enhanced extreme wind speeds over northern parts of central and westernEurope, and a decrease in extreme wind speeds in southern Europe.70 Climate change, impacts and vulnerability in Europe 2012
Changes in the climate systemclosely associated with atmospheric fronts whichdelineate changes in temperature, moisture, windspeed and direction, and atmospheric pressure. Innorthern and north-western Europe severe cyclonescan occur all year. In central Europe severe cyclonesoccur mainly between November and Februarywhereas weaker cyclones can also occur in otherseasons.north‐western European during the 1880s, followedby below average conditions between the 1930s and1960s, a pronounced increase in storminess until themid-1990s, and average or below activity afterwards.Somewhat similar patterns were observed in otherparts of Europe.Studies of storm activity have increased in recentyears as a result of improved observationaldatasets and the development of algorithms for theidentification and quantification of these phenomena(Ulbrich et al., 2009). In addition, high-resolutionGCM simulations for both present-day climateand climate change scenarios are increasinglybecoming available (van der Linden and Mitchell,2009). Nevertheless, there are still considerableuncertainties in our understanding of the processesinfluencing current storm activity and how thesemay be affected by climate change (Bengtsson et al.,2006; Pinto et al., 2007; Ulbrich et al., 2009).Storm events are associated with intense winds andprecipitation, which may lead to structural damage,flooding and storm surges (see Section 3.2.3 andChapter 5). These events can have large impacts onhuman health and on vulnerable systems, such asforests, and transport and energy infrastructures.According to the Munich Re NatCatSERVICE andthe EM-DAT database, storms were the costliestnatural hazard (in terms of insured losses) in Europebetween 1998 and 2009; they ranked fourth in termsof the number of human casualties (EEA, 2011b).Map 2.966 o60 o54 o48 o42 oTrends in the extreme windspeeds in the period 1871–2008based on reanalysisPast trendsStudies of past changes in extra-tropical storms haveused a variety of methods for analysing their activityin the storm track regions, making it difficult tocompare the results of different studies or to assessif there is any underlying climate change signal(Meehl et al., 2007; Ulbrich et al., 2009; Wang et al.,2011). Storm location and intensity in Europe hasshown considerable variation over the past century.Locally, increases in maximum gust wind speedshave been observed over recent decades (Usbecket al., 2010) but there is evidence for decreases instorm frequency since the 1990s (Ulbrich et al.,2009). Wind data at the local or regional levels canshow a series of decreases and increases continuingover several decades. Long records of wind speedfor various regions across Europe indicate thatstorminess has not significantly changed overthe past 200 years (Matulla et al., 2007). They alsoindicate relatively high levels of storminess in36 o 8 o W 0 o E 8 o 16 o 24 oTrends in the annual 95th percentile of daily maximumwind speeds, 1871–2008Note:Wind speed (m/s) α = 0.05– 0.2 – 0.15 – 0.1 – 0.05 0 0.05 0.1 0.15 0.2Gale day trends> 0.075 > 0.070 > 0.065 > 0.060 > 0.055Trends in the annual 95th percentile of daily maximumwind speeds in the 20th century reanalysis data set(ensemble mean) during the period 1871–2008.The trend is given in the units of the interannualstandard deviation and plotted only when significant.The coloured circles indicate trends in the number of'gale days' (an index that represents the number ofextremely windy days) over the period at the specificlocations.Source: Donat, Renggli, et al., 2011.Climate change, impacts and vulnerability in Europe 201271
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Changes <strong>in</strong> the climate systemMap 2.8Projected <strong>change</strong>s <strong>in</strong> 20-year maximum precipitation <strong>in</strong> summer <strong>and</strong> w<strong>in</strong>terSummerW<strong>in</strong>terProjected <strong>change</strong>s <strong>in</strong> 20-year maximum precipitation <strong>in</strong> summer <strong>and</strong> w<strong>in</strong>ter(%)– 40 – 20 0 20 40Note: Projected <strong>change</strong>s <strong>in</strong> 20-year maximum daily precipitation <strong>in</strong> summer (left) <strong>and</strong> w<strong>in</strong>ter (right) <strong>fr</strong>om 1961–1990 to 2071–2100based on the ensemble mean us<strong>in</strong>g a regional climate model (RCM) nested <strong>in</strong> 6 general circulation model (GCMs). Changesthat approximately lie outside of ± 10 % for the ensemble average are significant at the 10 % significance level.Source: Nikul<strong>in</strong> et al., 2011.2.2.6 StormsRelevanceStorms are atmospheric disturbances that aredef<strong>in</strong>ed by strong susta<strong>in</strong>ed w<strong>in</strong>d. In many cases,they are accompanied by heavy precipitation (ra<strong>in</strong>,hail or snow) <strong>and</strong> lightn<strong>in</strong>g. In <strong>Europe</strong>, storms canrange <strong>fr</strong>om relatively small <strong>and</strong> localised eventsto large features cover<strong>in</strong>g a substantial part of thecont<strong>in</strong>ent. They typically develop <strong>fr</strong>om extra-tropicalcyclones which are low-pressure weather systemsthat occur between 30 <strong>and</strong> 80 °N <strong>and</strong> capture theirenergy <strong>fr</strong>om the temperature contrast between thesub-tropical <strong>and</strong> polar air masses that meet <strong>in</strong> theAtlantic Ocean. These extra-tropical cyclones areKey messages: 2.2.6 Storms• Storm location, <strong>fr</strong>equency <strong>and</strong> <strong>in</strong>tensity have shown considerable variability across <strong>Europe</strong> over the pastcentury, mak<strong>in</strong>g it difficult to identify clear trends. A recent reanalysis suggests that storm<strong>in</strong>ess has<strong>in</strong>creased over the past century <strong>in</strong> northern <strong>and</strong> north-western <strong>Europe</strong> but this f<strong>in</strong>d<strong>in</strong>g is not yet robust.• <strong>Climate</strong> <strong>change</strong> projections for storms <strong>in</strong> the North Atlantic <strong>and</strong> <strong>Europe</strong> region show no clear consensus<strong>in</strong> either the direction of movement or the <strong>in</strong>tensity of storm activity. However, a recent study <strong>in</strong>volv<strong>in</strong>g20 climate models projects enhanced extreme w<strong>in</strong>d speeds over northern parts of central <strong>and</strong> western<strong>Europe</strong>, <strong>and</strong> a decrease <strong>in</strong> extreme w<strong>in</strong>d speeds <strong>in</strong> southern <strong>Europe</strong>.70 <strong>Climate</strong> <strong>change</strong>, <strong>impacts</strong> <strong>and</strong> <strong>vulnerability</strong> <strong>in</strong> <strong>Europe</strong> 2012