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

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Changes in the climate system2.2.2 Global and European temperatureRelevanceThis indicator summarises changes in averagenear‐surface temperature for the globe and for aregion covering the 39 EEA member and cooperatingcountries ( 39 ). Near-surface air temperature givesone of the clearest and most consistent signals ofglobal and regional climate change. A dense networkof stations across the globe, and particularly inEurope, provide regular monitoring of temperature,using standardised measurements, quality controland homogeneity procedures. Time series extendback for many decades or even centuries at somelocations.This indicator directly refers to the followingpolicy‐relevant questions ( 40 ):• Will the global average temperature increasestay within the EU and UNFCCC policy target of2.0 °C above pre-industrial levels?• Will the rate of global average temperatureincrease stay below the target of 0.2 °C increaseper decade?Global average annual temperature is expressedhere relative to a 'pre-industrial' period between1850 and 1899, which coincides with the beginningof widespread instrumental temperature records.During this time, anthropogenic GHGs from theindustrial revolution (between 1750 and 1850) areconsidered to have had a relatively small influenceon climate compared to natural influences. However,it should be noted that there is no rigorous scientificdefinition of the term 'pre-industrial climate' becausethe climate has also changed prior to 1850 due tointernal and forced natural variability.Key messages: 2.2.2 Global and European temperatureGlobal:• Three independent long records of global average near-surface (land and ocean) annual temperatureshow that the decade between 2002 and 2011 was 0.77 to 0.80 °C warmer than the pre-industrialaverage.• In recent decades, the rate of change in global average temperature has been close to the indicativelimit of 0.2 °C per decade.• The Arctic has warmed significantly more than the globe, and this is projected to continue into thefuture.• The best estimate for the further rise in global average temperature is between 1.8 and 4.0 °C for thelowest and highest SRES marker scenarios (IPCC SRES) that assume no additional political measures tolimit emissions. When climate model uncertainties are taken into account, the likely range increases to1.1–6.4 °C.• The EU target of limiting global average temperature increase to 2 °C above pre-industrial levels isprojected to be exceeded during the second half of this century and likely around 2050, for all six IPCCSRES emissions scenarios.Europe:• Annual average temperature across European land areas has warmed more than global averagetemperature, and slightly more than global land temperature. The average temperature for theEuropean land area for the last decade (2002–2011) is 1.3 °C above the pre-industrial level, whichmakes it the warmest decade on record.• Annual average land temperature over Europe is projected to continue increasing by more thanglobal average temperature during the 21st century. Increases in land temperature in Europe forthe SRES A1B emission scenario are projected between 1.0 and 2.5 °C by 2021–2050, and between2.5 and 4.0 °C by 2071–2100.• The largest temperature increases during the 21st century are projected over eastern and northernEurope in winter and over southern Europe in summer.( 39 ) In this section, EEA Europe is defined as the area between 35 °N to 70 °N and 25 °W to 30 °E, plus the area from 35 °N to 40 °Nand 30 °E to 45 °E (including also the Asian part of Turkey).( 40 ) The European Council proposed in its Sixth Environmental Action Programme (EC, 2002) that the global average temperatureincrease should be limited to not more than 2 °C above pre-industrial levels (about 1.3 °C above current global mean temperature).This limit was reaffirmed by the Environment Council and the European Council in 2005. Furthermore, the UNFCCC 15th Conferenceof the Parties (COP15) recognised, in the Copenhagen Accord (UNFCCC, 2009) the scientific evidence for the need to keep globalaverage temperature increase below 2 °C above pre-industrial levels (see Section 1.3). In addition, several studies have proposed tolimit the rate of anthropogenic warming to 0.2 °C per decade (WBGU, 2003; van Vliet and Leemans, 2005).56 Climate change, impacts and vulnerability in Europe 2012

Changes in the climate systemPast trendsGlobal:Since the end of the 19th century, records of globalaverage temperature have shown long-termwarming trends which have been especially rapid inthe most recent decades. Relative to pre-industrialtemperatures (taken here to be comparable with theearliest observations at the end of the 19th century),three independent analyses of global averagetemperature using near-surface observation records— HadCRUT3 (Brohan et al., 2006); NOAA-NCDC(Smith et al., 2008); and NASA-GISS (Hansen et al.,2010) — show similar amounts of warming by the2002 to 2011 decade of 0.77 °C, 0.78 °C and 0.80 °C,respectively (Figure 2.5 left). This magnitude ofwarming corresponds to more than one third of the2 °C warming permitted under the global climatestabilisation target of the EU and UNFCCC.Figure 2.5 (left) shows estimates (based oninstrumental measurements) of air temperatures at2 m height over land, and sea surface temperaturesobserved from ships and buoys. The variousestimates differ slightly because the underlyingsources differ in their methods for analysing thedata and filling data gaps. Another independentmethod that can be used to estimate changes inglobal average temperature is through 'Climatereanalysis' (see Box 2.2).The rate of change in global average temperatureduring the last century was on average around0.07 °C per decade (for all three analyses shownin Figure 2.5). The rate of change increased toaround 0.15 °C per decade averaged over the past50 years, and between 0.17 and 0.22 °C over the last20 years (Figure 2.5 right). This rate is close to theindicative limit of 0.2 °C per decade proposed bysome scientific studies (WBGU, 2003; van Vliet andLeemans, 2005).Figure 2.5 Change in global average temperature from three sources (1850–2011)Global average temperature change (°C)relative to pre-industrialRate of change (°C/decade)0.50.20.00.50.1– 0.50.0– 0.1– 1.01850 1900 1950 2000Met Office Hadley Centre and UEA ClimaticResearch UnitNOAA National Climatic Data CenterNASA Goddard Institute for Space Studies0.0– 0.21850 1900 1950 2000Met Office Hadley Centre and UEA ClimaticResearch UnitNOAA National Climatic Data CenterNASA Goddard Institute for Space StudiesNote:Change (left) and rates of change, based on 10-year running average (right) in global average air temperature. Temperatureis expressed in degrees Celsius (°C) relative to a pre-industrial baseline period. The upper time series on the left graph showsannual anomalies and the lower time series shows decadal average anomalies for the same datasets.Source: 1) Black line — HadCRUT3 from the UK Met Office Hadley Centre and University of East Anglia Climate Research Unit,baseline period 1850–1899 (Brohan et al., 2006). The grey area represents the 95 % confidence range.2) Red line — MLOST from the US National Oceanic and Atmospheric Administration (NOAA) National Climatic Data Center,baseline period 1880–1899 (Smith et al., 2008).3) Blue line — GISSTemp from the National Aeronautics and Space Administration (NASA) Goddard Institute for SpaceStudies, baseline period 1880–1899 (Hansen et al., 2010).Climate change, impacts and vulnerability in Europe 201257

Changes <strong>in</strong> the climate system2.2.2 Global <strong>and</strong> <strong>Europe</strong>an temperatureRelevanceThis <strong>in</strong>dicator summarises <strong>change</strong>s <strong>in</strong> averagenear‐surface temperature for the globe <strong>and</strong> for aregion cover<strong>in</strong>g the 39 EEA member <strong>and</strong> cooperat<strong>in</strong>gcountries ( 39 ). Near-surface air temperature givesone of the clearest <strong>and</strong> most consistent signals ofglobal <strong>and</strong> regional climate <strong>change</strong>. A dense networkof stations across the globe, <strong>and</strong> particularly <strong>in</strong><strong>Europe</strong>, provide regular monitor<strong>in</strong>g of temperature,us<strong>in</strong>g st<strong>and</strong>ardised measurements, quality control<strong>and</strong> homogeneity procedures. Time series extendback for many decades or even centuries at somelocations.This <strong>in</strong>dicator directly refers to the follow<strong>in</strong>gpolicy‐relevant questions ( 40 ):• Will the global average temperature <strong>in</strong>creasestay with<strong>in</strong> the EU <strong>and</strong> UNFCCC policy target of2.0 °C above pre-<strong>in</strong>dustrial levels?• Will the rate of global average temperature<strong>in</strong>crease stay below the target of 0.2 °C <strong>in</strong>creaseper decade?Global average annual temperature is expressedhere relative to a 'pre-<strong>in</strong>dustrial' period between1850 <strong>and</strong> 1899, which co<strong>in</strong>cides with the beg<strong>in</strong>n<strong>in</strong>gof widespread <strong>in</strong>strumental temperature records.Dur<strong>in</strong>g this time, anthropogenic GHGs <strong>fr</strong>om the<strong>in</strong>dustrial revolution (between 1750 <strong>and</strong> 1850) areconsidered to have had a relatively small <strong>in</strong>fluenceon climate compared to natural <strong>in</strong>fluences. However,it should be noted that there is no rigorous scientificdef<strong>in</strong>ition of the term 'pre-<strong>in</strong>dustrial climate' becausethe climate has also <strong>change</strong>d prior to 1850 due to<strong>in</strong>ternal <strong>and</strong> forced natural variability.Key messages: 2.2.2 Global <strong>and</strong> <strong>Europe</strong>an temperatureGlobal:• Three <strong>in</strong>dependent long records of global average near-surface (l<strong>and</strong> <strong>and</strong> ocean) annual temperatureshow that the decade between 2002 <strong>and</strong> 2011 was 0.77 to 0.80 °C warmer than the pre-<strong>in</strong>dustrialaverage.• In recent decades, the rate of <strong>change</strong> <strong>in</strong> global average temperature has been close to the <strong>in</strong>dicativelimit of 0.2 °C per decade.• The Arctic has warmed significantly more than the globe, <strong>and</strong> this is projected to cont<strong>in</strong>ue <strong>in</strong>to thefuture.• The best estimate for the further rise <strong>in</strong> global average temperature is between 1.8 <strong>and</strong> 4.0 °C for thelowest <strong>and</strong> highest SRES marker scenarios (IPCC SRES) that assume no additional political measures tolimit emissions. When climate model uncerta<strong>in</strong>ties are taken <strong>in</strong>to account, the likely range <strong>in</strong>creases to1.1–6.4 °C.• The EU target of limit<strong>in</strong>g global average temperature <strong>in</strong>crease to 2 °C above pre-<strong>in</strong>dustrial levels isprojected to be exceeded dur<strong>in</strong>g the second half of this century <strong>and</strong> likely around 2050, for all six IPCCSRES emissions scenarios.<strong>Europe</strong>:• Annual average temperature across <strong>Europe</strong>an l<strong>and</strong> areas has warmed more than global averagetemperature, <strong>and</strong> slightly more than global l<strong>and</strong> temperature. The average temperature for the<strong>Europe</strong>an l<strong>and</strong> area for the last decade (2002–2011) is 1.3 °C above the pre-<strong>in</strong>dustrial level, whichmakes it the warmest decade on record.• Annual average l<strong>and</strong> temperature over <strong>Europe</strong> is projected to cont<strong>in</strong>ue <strong>in</strong>creas<strong>in</strong>g by more thanglobal average temperature dur<strong>in</strong>g the 21st century. Increases <strong>in</strong> l<strong>and</strong> temperature <strong>in</strong> <strong>Europe</strong> forthe SRES A1B emission scenario are projected between 1.0 <strong>and</strong> 2.5 °C by 2021–2050, <strong>and</strong> between2.5 <strong>and</strong> 4.0 °C by 2071–2100.• The largest temperature <strong>in</strong>creases dur<strong>in</strong>g the 21st century are projected over eastern <strong>and</strong> northern<strong>Europe</strong> <strong>in</strong> w<strong>in</strong>ter <strong>and</strong> over southern <strong>Europe</strong> <strong>in</strong> summer.( 39 ) In this section, EEA <strong>Europe</strong> is def<strong>in</strong>ed as the area between 35 °N to 70 °N <strong>and</strong> 25 °W to 30 °E, plus the area <strong>fr</strong>om 35 °N to 40 °N<strong>and</strong> 30 °E to 45 °E (<strong>in</strong>clud<strong>in</strong>g also the Asian part of Turkey).( 40 ) The <strong>Europe</strong>an Council proposed <strong>in</strong> its Sixth Environmental Action Programme (EC, 2002) that the global average temperature<strong>in</strong>crease should be limited to not more than 2 °C above pre-<strong>in</strong>dustrial levels (about 1.3 °C above current global mean temperature).This limit was reaffirmed by the Environment Council <strong>and</strong> the <strong>Europe</strong>an Council <strong>in</strong> 2005. Furthermore, the UNFCCC 15th Conferenceof the Parties (COP15) recognised, <strong>in</strong> the Copenhagen Accord (UNFCCC, 2009) the scientific evidence for the need to keep globalaverage temperature <strong>in</strong>crease below 2 °C above pre-<strong>in</strong>dustrial levels (see Section 1.3). In addition, several studies have proposed tolimit the rate of anthropogenic warm<strong>in</strong>g to 0.2 °C per decade (WBGU, 2003; van Vliet <strong>and</strong> Leemans, 2005).56 <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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