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 socio-economic systems and healthcan also enhance the risk of forest decline, ifcritical loads are exceeded. The concentrationsof nitrogen oxides due to fossil fuel combustionare still high in spite of increased use of catalyticconvertors. The high concentrations of reducednitrogen from intensive agriculture, like ammoniaare still a matter of concern for forests in the aircausing eutrophication (Sutton, 2011). Increasesin ground‐level ozone are likely in some regionsdue to warmer temperatures, which would cause adecrease in forest health and growth, which in turnhas critical implications for forest distributions andfuture rates of carbon sequestration (Matyssek et al.,2012).In general, forest productivity is projected toincrease in areas with increased water availability,if appropriate tree species are growing there, whileit is projected to decrease where water is scarce andprojected to decline further. Wherever droughtsincrease, forest productivity is expected to decrease.Overall, climate change is projected to have a positiveeffect on the growing stocks in northern Europe anda negative effect in some regions in southern Europe.However, quantitative projections are not currentlyavailable as existing studies on future climate impactson forests focus on effects on individual species.Box 4.1 provides quantitative projections of forestcomposition and their economic impacts.Box 4.1Projected changes in forest composition and their economic impactsClimate change is expected to strongly affect the biological and economic viability of different tree species inEurope. A recent modelling study assessed the impacts of projected climate change on forest composition acrossEurope as well as the economic consequences in terms of annual productivity and land value (Hanewinkel et al.,2012). The major commercial tree species in Europe, Norway spruce, shifts northward and to higher altitude.It loses large parts of its present range in central, eastern and western Europe under all climate scenarios(SRES A1B, A1FI, and B2). Depending on the emission scenario and climate model, between 21 % and 60 %(mean: 34 %) of European forest lands will be suitable only for a Mediterranean oak forest type with low economicreturns by 2100, compared to 11 % in the baseline period 1961–1990. Further information on major groups oftree species is provided in Figure 4.2. As a result of the decline of economically valuable species, the value offorest land in Europe is projected to decrease between 14 % and 50 % (mean: 28 % for an interest rate of 2 %)by 2100. The economic loss is estimated at several hundred billion EUR.Figure 4.2Projected change in the share of major tree species in EuropeNote:The bars reflect the standard deviation resulting from four different climate model realisations of the SRES A1B emissionscenario. The relative size of the icons corresponds to the relative height of mature trees of the species groups.For additional information see the original reference. Europe refers to the area covered by the ENSEMBLE climateprojections.Source: Hanewinkel et al., 2012. © Nature Publishing Group. Reprinted with permission.176 Climate change, impacts and vulnerability in Europe 2012
Climate impacts on socio-economic systems and health4.2.3 Forest firesRelevanceForest fires are an integral part of forest ecosystemdynamics in many ecosystems where they arean essential element of forest renewal. They helpcontrol insect and disease damage and eliminatelitter that has accumulated on forest floors. At thesame time, forest fires are an important disturbanceagent in many forested landscapes. Fire risk dependson many factors such as weather, vegetation(e.g. fuel load and condition), topography, forestmanagement practices and socio‐economic context,to mention the main ones. Extreme fire episodes anddevastating fire seasons of recent years in Europewere in most cases driven by severe fire weatherconditions. Although most of the wild fires inEurope are ignited by humans (either accidently orintentionally), it is widely recognised that weatherconditions and accumulation of fuel play a dominantrole in affecting the changes in fire risk over time.Thus climate change is expected to have a strongimpact on forest fire regimes in Europe.Past trendsHistorical fire series are available in Europe andregularly updated within EFFIS. However, the timeperiod covered is not the same for all countries andonly in a few case series is longer than 25 yearsavailable. A long time series of forest fire data isavailable for five particularly affected countries insouthern Europe (Greece, Spain, France, Italy andPortugal). The total burnt area per year in the fivesouthern Member States since 1980 is shown onFigure 4.3. Since the area of each country is different,and the area at risk within each country is alsodifferent, comparisons among countries cannot beabsolute.The statistics vary considerably from one year to thenext, which clearly indicates how much the burntarea depends on seasonal meteorological conditions.Some multi-annual periodicity in the burned areatrend can also be partially attributed to the deadbiomass burning/accumulation cycle typical of thefire-prone regions. The historical trend of numberof fires is more controversial to analyse becausefire frequency is strongly affected by the significantchanges that occurred in past years in the statisticalreporting systems of the countries. Reported firefrequency in southern European countries hasincreased during the 1990s to then stabilise foraround one decade and slightly decrease duringrecent years.To complement the information from past forestfires, past trends of fire danger have also beenanalysed processing series of meteorological firedanger indices, which are routinely used to ratethe fire potential due to weather conditions. TheCanadian Fire Weather Index (FWI) is used inEFFIS to rate the daily fire danger conditions inEurope. FWI can be transformed with a simpleequation into a daily severity rating index which isdeemed to be linearly related with fire suppressiondifficulties (Van Wagner, 1987). Daily severity valuescan be averaged over the fire season obtaining aSeasonal Severity Rating (SSR) index, which allowsobjective comparison of fire danger from year toyear and from region to region. Although the indexis dimensionless and mainly used for comparisonpurposes, SSR values above 6 may be considered inthe extreme range. Weather input to compute SSRare the same as for FWI (air temperature, relativehumidity, wind, precipitation). Other driving factorsof fire regimes, such as land-use changes or fueldynamics, are not taken into account by SSR whichis based on weather parameters. However, thefundamental role played by weather in affecting theKey messages: 4.2.3 Forest fires• Fire risk depends on many factors, including climatic conditions, vegetation (e.g. fuel load andcondition), forest management practices and other socio‐economic factors.• The number of fires in the Mediterranean region has increased over the period from 1980 to 2000;it has decreased thereafter.• In a warmer climate, more severe fire weather and an expansion of the fire-prone area and longer fireseasons, as a consequence, are projected, but with considerable regional variation.• The impact of fire events is particularly strong in southern Europe on already degraded ecosystems.Climate change, impacts and vulnerability in Europe 2012177
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<strong>Climate</strong> <strong>impacts</strong> on socio-economic systems <strong>and</strong> health4.2.3 Forest firesRelevanceForest fires are an <strong>in</strong>tegral part of forest ecosystemdynamics <strong>in</strong> many ecosystems where they arean essential element of forest renewal. They helpcontrol <strong>in</strong>sect <strong>and</strong> disease damage <strong>and</strong> elim<strong>in</strong>atelitter that has accumulated on forest floors. At thesame time, forest fires are an important disturbanceagent <strong>in</strong> many forested l<strong>and</strong>scapes. Fire risk dependson many factors such as weather, vegetation(e.g. fuel load <strong>and</strong> condition), topography, forestmanagement practices <strong>and</strong> socio‐economic context,to mention the ma<strong>in</strong> ones. Extreme fire episodes <strong>and</strong>devastat<strong>in</strong>g fire seasons of recent years <strong>in</strong> <strong>Europe</strong>were <strong>in</strong> most cases driven by severe fire weatherconditions. Although most of the wild fires <strong>in</strong><strong>Europe</strong> are ignited by humans (either accidently or<strong>in</strong>tentionally), it is widely recognised that weatherconditions <strong>and</strong> accumulation of fuel play a dom<strong>in</strong>antrole <strong>in</strong> affect<strong>in</strong>g the <strong>change</strong>s <strong>in</strong> fire risk over time.Thus climate <strong>change</strong> is expected to have a strongimpact on forest fire regimes <strong>in</strong> <strong>Europe</strong>.Past trendsHistorical fire series are available <strong>in</strong> <strong>Europe</strong> <strong>and</strong>regularly updated with<strong>in</strong> EFFIS. However, the timeperiod covered is not the same for all countries <strong>and</strong>only <strong>in</strong> a few case series is longer than 25 yearsavailable. A long time series of forest fire data isavailable for five particularly affected countries <strong>in</strong>southern <strong>Europe</strong> (Greece, Spa<strong>in</strong>, France, Italy <strong>and</strong>Portugal). The total burnt area per year <strong>in</strong> the fivesouthern Member States s<strong>in</strong>ce 1980 is shown onFigure 4.3. S<strong>in</strong>ce the area of each country is different,<strong>and</strong> the area at risk with<strong>in</strong> each country is alsodifferent, comparisons among countries cannot beabsolute.The statistics vary considerably <strong>fr</strong>om one year to thenext, which clearly <strong>in</strong>dicates how much the burntarea depends on seasonal meteorological conditions.Some multi-annual periodicity <strong>in</strong> the burned areatrend can also be partially attributed to the deadbiomass burn<strong>in</strong>g/accumulation cycle typical of thefire-prone regions. The historical trend of numberof fires is more controversial to analyse becausefire <strong>fr</strong>equency is strongly affected by the significant<strong>change</strong>s that occurred <strong>in</strong> past years <strong>in</strong> the statisticalreport<strong>in</strong>g systems of the countries. Reported fire<strong>fr</strong>equency <strong>in</strong> southern <strong>Europe</strong>an countries has<strong>in</strong>creased dur<strong>in</strong>g the 1990s to then stabilise foraround one decade <strong>and</strong> slightly decrease dur<strong>in</strong>grecent years.To complement the <strong>in</strong>formation <strong>fr</strong>om past forestfires, past trends of fire danger have also beenanalysed process<strong>in</strong>g series of meteorological firedanger <strong>in</strong>dices, which are rout<strong>in</strong>ely used to ratethe fire potential due to weather conditions. TheCanadian Fire Weather Index (FWI) is used <strong>in</strong>EFFIS to rate the daily fire danger conditions <strong>in</strong><strong>Europe</strong>. FWI can be transformed with a simpleequation <strong>in</strong>to a daily severity rat<strong>in</strong>g <strong>in</strong>dex which isdeemed to be l<strong>in</strong>early related with fire suppressiondifficulties (Van Wagner, 1987). Daily severity valuescan be averaged over the fire season obta<strong>in</strong><strong>in</strong>g aSeasonal Severity Rat<strong>in</strong>g (SSR) <strong>in</strong>dex, which allowsobjective comparison of fire danger <strong>fr</strong>om year toyear <strong>and</strong> <strong>fr</strong>om region to region. Although the <strong>in</strong>dexis dimensionless <strong>and</strong> ma<strong>in</strong>ly used for comparisonpurposes, SSR values above 6 may be considered <strong>in</strong>the extreme range. Weather <strong>in</strong>put to compute SSRare the same as for FWI (air temperature, relativehumidity, w<strong>in</strong>d, precipitation). Other driv<strong>in</strong>g factorsof fire regimes, such as l<strong>and</strong>-use <strong>change</strong>s or fueldynamics, are not taken <strong>in</strong>to account by SSR whichis based on weather parameters. However, thefundamental role played by weather <strong>in</strong> affect<strong>in</strong>g theKey messages: 4.2.3 Forest fires• Fire risk depends on many factors, <strong>in</strong>clud<strong>in</strong>g climatic conditions, vegetation (e.g. fuel load <strong>and</strong>condition), forest management practices <strong>and</strong> other socio‐economic factors.• The number of fires <strong>in</strong> the Mediterranean region has <strong>in</strong>creased over the period <strong>fr</strong>om 1980 to 2000;it has decreased thereafter.• In a warmer climate, more severe fire weather <strong>and</strong> an expansion of the fire-prone area <strong>and</strong> longer fireseasons, as a consequence, are projected, but with considerable regional variation.• The impact of fire events is particularly strong <strong>in</strong> southern <strong>Europe</strong> on already degraded ecosystems.<strong>Climate</strong> <strong>change</strong>, <strong>impacts</strong> <strong>and</strong> <strong>vulnerability</strong> <strong>in</strong> <strong>Europe</strong> 2012177