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
Climate impacts on environmental systemsMap 3.10Projected change in minimum river flow with return period of 20 years-30° a) 2020s -10° 0° 10° 20° 30° 40° 50° -30° b) 2050s -10° 0° 10° 20° 30° 40° 50° -30° c) 2080s -10°0°10°20°30°40°50°60° 60°60° 60°60° 60°50° 50°50° 50°50° 50°40° 40°40° 40°40° 40°0°10°20°0°10°20°0°10°20°Relative change in minimum river flow with return period of 20 years between future period and 1961–1990 (SRES A1B)(%)– 60 – 40 – 20 – 10 – 5 5 10 20 40 60© 2012 JRC, European CommissionNote:Relative change in minimum river flow for a) 2020s, b) 2050s and c) 2080s compared to 1961–1990 for SRES A1B scenario.Source: Rojas et al., 2012.3.3.5 Water temperatureRelevanceWater temperature is one of the parameters thatdetermine the overall health of aquatic ecosystems.Most aquatic organisms have a specific range oftemperatures they can tolerate, which determinestheir spatial distribution. Changes in temperaturealso determine ice cover periods, thermalstratification of lakes, nutrient availability and theduration of growing seasons that in turn affectspecies composition and food web structures.Past trendsThe surface water temperatures of major riversin Europe have increased by 1–3 °C over the lastcentury (Figure 3.10). For example, the averagetemperature in the Rhine near Basel has risen bymore than 2 °C in the last 50 years (FOEN, 2011). Thetemperature of the downstream part of the Rhineincreased by 3 °C between 1910 and 2010. Two thirdsof the increase at the downstream Rhine is attributedto the increased use of cooling water and onethird to the increase in air temperature as a resultof climate change (Bresser et al., 2006). A similarKey messages: 3.3.5 Water temperature• Water temperatures in major European rivers have increased by 1–3 °C over the last century. Severaltime series show increasing lake and river temperatures all over Europe over the last 60 to 90 years.• Lake and river surface water temperatures are projected to increase with further projected increases inair temperature.• Increased temperature can result in marked changes in species composition and functioning of aquaticecosystems.122 Climate change, impacts and vulnerability in Europe 2012
Climate impacts on environmental systemsFigure 3.10 Trends in water temperature of large European rivers and lakes in the20th century°C25201510501900 1920 1940 1960 1980 2000Rhine, Lobith Danube, Vienna Meuse, EijsdenLake Saimaa, FinlandLake Võrtsjärv, EstoniaNote:Annual average water temperature in River Rhine and River Meuse (1911–2010); River Danube (1901–1998), Lake Võrtsjärv(1947–2011), and average water temperature in August in Lake Saimaa, Finland (1924–2011).Source: River Rhine and River Meuse: Compendium voor de Leefomgeving, 2012; River Danube: Hohensinner, 2006 (personalcommunication); Lake Saimaa: Johanne Korhonen, 2012 (personal communication); Lake Võrtsjärv: Peeter Nõges, 2012(personal communication).increase has been observed in the Meuse. The annualaverage temperature of the Danube increased byaround by 1 °C during the last century. Increases insurface water temperature were also found in somelarge lakes. Lake Võrtsjärv in Estonia had a 0.7 °Cincrease between 1947 and 2011, and the summer(August) water temperature of Lake Saimaa, Finlandincreased more than 1 °C over the last century.Several time series indicate a general trend ofincreasing water temperature in European riversand lakes in the range of 0.05 to 0.8 °C per decade(Dabrowski et al., 2004; George and Hurley, 2004;Pernaravièiûtë, 2004; Bresser et al., 2006). Thesurface water temperature of some rivers and lakesin Switzerland has increased by more than 2 °Csince 1950 (BUWAL, 2004; Hari et al., 2006). In thelarge lakes in the Alps the water temperature hasgenerally increased by 0.1–0.3 °C per decade: LakeMaggiore and other large Italian lakes (Ambrosettiand Barbanti, 1999; Livingstone, 2003; Annevilleet al., 2005; Dokulil et al., 2006).ProjectionsLake surface water temperatures are projectedto increase further, in parallel with the projectedincreases in air temperature. The exact amountof warming depends on the magnitude of globalwarming, on the region, on the season and onlake properties (Malmaeus et al., 2006; Georgeet al., 2007). Physical modelling studies predictthat temperatures will increase more in the upperregions of the water column than in the lowerregions, resulting in generally steeper verticaltemperature gradients and enhanced thermalstability (Peeters et al., 2002). Such increased lakethermal stability was observed both in Switzerlandduring the mild 2006/2007 winter (Rempfer et al.,2010) and in Italy during the hot 2009 summer(Nõges et al., 2011). Further impacts of increasedlake and river water temperature are described inSection 3.3.6.Climate change, impacts and vulnerability in Europe 2012123
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<strong>Climate</strong> <strong>impacts</strong> on environmental systemsMap 3.10Projected <strong>change</strong> <strong>in</strong> m<strong>in</strong>imum river flow with return period of 20 years-30° a) 2020s -10° 0° 10° 20° 30° 40° 50° -30° b) 2050s -10° 0° 10° 20° 30° 40° 50° -30° c) 2080s -10°0°10°20°30°40°50°60° 60°60° 60°60° 60°50° 50°50° 50°50° 50°40° 40°40° 40°40° 40°0°10°20°0°10°20°0°10°20°Relative <strong>change</strong> <strong>in</strong> m<strong>in</strong>imum river flow with return period of 20 years between future period <strong>and</strong> 1961–1990 (SRES A1B)(%)– 60 – 40 – 20 – 10 – 5 5 10 20 40 60© 2012 JRC, <strong>Europe</strong>an CommissionNote:Relative <strong>change</strong> <strong>in</strong> m<strong>in</strong>imum river flow for a) 2020s, b) 2050s <strong>and</strong> c) 2080s compared to 1961–1990 for SRES A1B scenario.Source: Rojas et al., 2012.3.3.5 Water temperatureRelevanceWater temperature is one of the parameters thatdeterm<strong>in</strong>e the overall health of aquatic ecosystems.Most aquatic organisms have a specific range oftemperatures they can tolerate, which determ<strong>in</strong>estheir spatial distribution. Changes <strong>in</strong> temperaturealso determ<strong>in</strong>e ice cover periods, thermalstratification of lakes, nutrient availability <strong>and</strong> theduration of grow<strong>in</strong>g seasons that <strong>in</strong> turn affectspecies composition <strong>and</strong> food web structures.Past trendsThe surface water temperatures of major rivers<strong>in</strong> <strong>Europe</strong> have <strong>in</strong>creased by 1–3 °C over the lastcentury (Figure 3.10). For example, the averagetemperature <strong>in</strong> the Rh<strong>in</strong>e near Basel has risen bymore than 2 °C <strong>in</strong> the last 50 years (FOEN, 2011). Thetemperature of the downstream part of the Rh<strong>in</strong>e<strong>in</strong>creased by 3 °C between 1910 <strong>and</strong> 2010. Two thirdsof the <strong>in</strong>crease at the downstream Rh<strong>in</strong>e is attributedto the <strong>in</strong>creased use of cool<strong>in</strong>g water <strong>and</strong> onethird to the <strong>in</strong>crease <strong>in</strong> air temperature as a resultof climate <strong>change</strong> (Bresser et al., 2006). A similarKey messages: 3.3.5 Water temperature• Water temperatures <strong>in</strong> major <strong>Europe</strong>an rivers have <strong>in</strong>creased by 1–3 °C over the last century. Severaltime series show <strong>in</strong>creas<strong>in</strong>g lake <strong>and</strong> river temperatures all over <strong>Europe</strong> over the last 60 to 90 years.• Lake <strong>and</strong> river surface water temperatures are projected to <strong>in</strong>crease with further projected <strong>in</strong>creases <strong>in</strong>air temperature.• Increased temperature can result <strong>in</strong> marked <strong>change</strong>s <strong>in</strong> species composition <strong>and</strong> function<strong>in</strong>g of aquaticecosystems.122 <strong>Climate</strong> <strong>change</strong>, <strong>impacts</strong> <strong>and</strong> <strong>vulnerability</strong> <strong>in</strong> <strong>Europe</strong> 2012