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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 systems3.5.5 Biomass production <strong>and</strong> recurrent negativeprecipitation anomaliesSoil degradation processes are global phenomenathat cause a reduc<strong>in</strong>g biophysical capacity <strong>in</strong> thel<strong>and</strong> to susta<strong>in</strong>ably produce ecosystems services <strong>and</strong>economic value. They are l<strong>in</strong>ked to complex patternsof l<strong>and</strong> use <strong>and</strong> climatic variations. Observed<strong>change</strong>s <strong>in</strong> primary productivity of ecosystemsare a strong <strong>in</strong>dication of the onset or <strong>in</strong>creas<strong>in</strong>g<strong>vulnerability</strong> to soil degradation. As discussed<strong>in</strong> Section 3.5.2, organic matter is an importantdriver of several soil functions. A reduction <strong>in</strong> theproduction of biomass will have an impact on soilorganic matter levels <strong>and</strong> related nutrient cycles. Inparticular the parallel reduction <strong>in</strong> the vegetativecover <strong>and</strong> plant roots will <strong>in</strong>crease the risk of bothw<strong>in</strong>d <strong>and</strong> water erosion.Climatic conditions <strong>and</strong> <strong>in</strong>tensive agriculture makethe Mediterranean region particularly vulnerableto soil degradation. Ever more dem<strong>and</strong><strong>in</strong>g l<strong>and</strong> useleads to water scarcity, limit<strong>in</strong>g several ecosystemservices normally provided by soil. Amplifiedvariability of aridity limits the ability of <strong>in</strong>tensivelyused human-environment systems to recover <strong>fr</strong>omspecific pressures such as sal<strong>in</strong>isation, drought<strong>and</strong> fire (see Section 4.1). In turn, this leads to an<strong>in</strong>crease <strong>in</strong> soil degradation <strong>and</strong>, <strong>in</strong> extreme cases,desertification.Map 3.24 presents areas affected by three recurrentnegative precipitation anomalies over a period of10 years, <strong>and</strong> as such provides a first <strong>in</strong>dicationof areas under risk of soil degradation. Many soiltypes <strong>in</strong> the Mediterranean region already showsymptoms of degradation (i.e. shallow depth,low soil organic carbon content, prone to erosion,low fertility, <strong>in</strong>creased sal<strong>in</strong>ity <strong>and</strong> forest fires)which, together with the hot, dry climate of theregion, hampers the assessment of ongo<strong>in</strong>g l<strong>and</strong>degradation.While the effects of reduced biomass productionmay be dramatic <strong>in</strong> the Mediterranean region,the consequences on soil resources may also beevident <strong>in</strong> more temperate or humid regions.Recent observations suggest that Mediterraneanecosystems are generally resilient <strong>and</strong> resistant todroughts. However, where human activity becomestoo <strong>in</strong>tense, degradation is more pronounced<strong>and</strong> can possibly become irreversible. Map 3.24illustrates that, even after recurrent droughts, theMediterranean environment recovers well, apart<strong>fr</strong>om areas that are under <strong>in</strong>tense agriculturaluse <strong>and</strong> where the erosion risk is already high(see Map 3.21).Projections are very limited. Increases <strong>in</strong> therecurrence of extreme events, such as droughts,comb<strong>in</strong>ed with risks, such as forest fires, <strong>and</strong> anexpansion of <strong>in</strong>tensive l<strong>and</strong> use will probably <strong>in</strong>ducehigher levels of degradation, <strong>in</strong>clud<strong>in</strong>g soil erosion<strong>and</strong>, <strong>in</strong> turn, reduce the quality <strong>and</strong> availability ofnatural resources <strong>and</strong> ecosystems services.Key messages: 3.5.5 Biomass production <strong>and</strong> recurrent negative precipitation anomalies• Biomass production is a major soil function <strong>and</strong> its decl<strong>in</strong>e can be used as a proxy for soil degradation.• Recurrence of negative precipitation anomalies is lead<strong>in</strong>g to an <strong>in</strong>creased risk of soil degradation dueto the reduction of biomass, which is the ma<strong>in</strong> source of soil organic matter <strong>and</strong> protects soils <strong>fr</strong>omerosion.• Soil degradation processes are already <strong>in</strong>tense <strong>in</strong> several parts of the Mediterranean <strong>and</strong> <strong>in</strong> some partsof central-eastern <strong>Europe</strong>.• In many cases, <strong>in</strong>creased human pressure aggravated by climate <strong>change</strong> <strong>impacts</strong> can lead toirreversible soil degradation processes with adverse social, economic <strong>and</strong> environmental effects.• Increase <strong>in</strong> recurrence of extreme climate events, such as droughts, comb<strong>in</strong>ed with specific hazards,such as fires <strong>and</strong> both natural <strong>and</strong> human-<strong>in</strong>duced sal<strong>in</strong>ity, <strong>and</strong>/or an expansion of <strong>in</strong>tensive l<strong>and</strong> use orl<strong>and</strong>-use <strong>change</strong>, will probably <strong>in</strong>duce higher levels of l<strong>and</strong> degradation.156 <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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