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Climate change impacts and vulnerability in Europe 2016

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Changes <strong>in</strong> the climate system<br />

more <strong>in</strong>tense for RCP8.5 than for RCP2.6. The warm<strong>in</strong>g<br />

is particularly strong at high latitudes. Increas<strong>in</strong>g<br />

precipitation is projected for high-latitude regions <strong>and</strong><br />

the equatorial Pacific, whereas decreas<strong>in</strong>g precipitation<br />

is projected for many sub-tropical <strong>and</strong> mid-latitude<br />

regions, <strong>in</strong>clud<strong>in</strong>g the Mediterranean.<br />

GCMs provide guidance on the range of possible futures<br />

for each scenario. For example, Figure 3.4 depicts key<br />

aspects of future climate <strong>change</strong> <strong>in</strong> <strong>Europe</strong> for two<br />

future periods <strong>and</strong> two scenarios. Key uncerta<strong>in</strong>ties<br />

(see Section 1.4 for further explanation) are depicted by<br />

show<strong>in</strong>g the results for two RCP scenarios (RCP2.6 <strong>and</strong><br />

RCP8.5) <strong>and</strong> for several GCMs separately.<br />

All models <strong>and</strong> both scenarios show that <strong>Europe</strong> will<br />

become warmer <strong>in</strong> the 21st century. For the 2040s,<br />

both scenarios (RCP2.6 <strong>and</strong> RCP8.5) show similar<br />

<strong>change</strong>s <strong>in</strong> precipitation, <strong>and</strong> the differences are<br />

ma<strong>in</strong>ly the result of model uncerta<strong>in</strong>ties. However,<br />

<strong>in</strong> the 2080s, the difference between both scenarios<br />

<strong>in</strong>creases. Almost all climate models agree that<br />

northern <strong>Europe</strong> (top of Figure 3.4) will become wetter,<br />

<strong>in</strong> particular under the RCP8.5 scenario. Under the<br />

RCP8.5 scenario, all models agree that southern <strong>Europe</strong><br />

will become drier <strong>in</strong> the 2080s (bottom of Figure 3.4).<br />

However, under the RCP2.6 scenario, the GCMs do<br />

not agree on the direction of <strong>change</strong>s <strong>in</strong> both future<br />

periods.<br />

Map 3.2<br />

Projected <strong>change</strong>s <strong>in</strong> global average surface temperature <strong>and</strong> precipitation<br />

RCP2.6<br />

RCP2.6<br />

RCP8.5<br />

RCP8.5<br />

Changes <strong>in</strong> global average surface temperature (left) <strong>and</strong> precipitation (right) <strong>in</strong> 2081–2100 relative to 1986–2005 under RCP2.6<br />

(upper panel) <strong>and</strong> RCP8.5 (lower panel)<br />

ºC<br />

–2 – 1.5 – 1 – 0.5 0 0.5 1 1.5 2 3 4 5 7 9 11<br />

%<br />

– 50 – 40 – 30 – 20 – 10 0 10 20<br />

30 40 50<br />

Regions where the multi–model mean signal is less than 1 st<strong>and</strong>ard deviation of <strong>in</strong>ternal variability<br />

Regions where the multi–model mean signal is greater than 2 st<strong>and</strong>ard deviations of <strong>in</strong>ternal variability <strong>and</strong> where 90 % of models<br />

agree on the sign of <strong>change</strong><br />

Note:<br />

Source:<br />

Hatch<strong>in</strong>g <strong>in</strong>dicates regions where the multi-model mean signal is less than one st<strong>and</strong>ard deviation of <strong>in</strong>ternal variability. Stippl<strong>in</strong>g<br />

<strong>in</strong>dicates regions where the multi-model mean signal is greater than two st<strong>and</strong>ard deviations of <strong>in</strong>ternal variability <strong>and</strong> where 90 % of<br />

models agree on the direction of <strong>change</strong>.<br />

IPCC, 2013b (Figure SPM.8.a/b). © 2013 Intergovernmental Panel on <strong>Climate</strong> Change. Reproduced with permission.<br />

<strong>Climate</strong> <strong>change</strong>, <strong>impacts</strong> <strong>and</strong> <strong>vulnerability</strong> <strong>in</strong> <strong>Europe</strong> <strong>2016</strong> | An <strong>in</strong>dicator-based report<br />

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