26.01.2017 Views

Climate change impacts and vulnerability in Europe 2016

document

document

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

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

Map 3.5 Observed trends <strong>in</strong> warm days across <strong>Europe</strong> between 1960 <strong>and</strong> 2015<br />

-30°<br />

-20°<br />

-10°<br />

0°<br />

10°<br />

20°<br />

30°<br />

40°<br />

50°<br />

60°<br />

70°<br />

Observed trends <strong>in</strong> warm<br />

days across <strong>Europe</strong> between<br />

1960 <strong>and</strong> 2015<br />

Days/decade<br />

0–1<br />

1–2<br />

60°<br />

2–3<br />

3–4<br />

50°<br />

4–5<br />

5–6<br />

6–7<br />

7–8<br />

50°<br />

8–9<br />

9–10<br />

10–11<br />

40°<br />

No data<br />

Outside coverage<br />

40°<br />

0 500 1000 1500 km<br />

0°<br />

10°<br />

20°<br />

30°<br />

40°<br />

Note:<br />

Warm days are def<strong>in</strong>ed as be<strong>in</strong>g above the 90th percentile of the daily maximum temperature centred on a five-day w<strong>in</strong>dow for a<br />

reference period. Grid boxes outl<strong>in</strong>ed with solid black l<strong>in</strong>es conta<strong>in</strong> at least three stations <strong>and</strong> thus trends are more robust. High<br />

confidence <strong>in</strong> the long-term trend (at the 5 % level) is shown by a black dot (which is the case for all grid boxes <strong>in</strong> this map). The<br />

reference period is 1971–2000.<br />

Source: EEA <strong>and</strong> UK Met Office, based on HadEX2 (updated from Donat, Alex<strong>and</strong>er, Yang, Durre, Vose, Dunn et al., 2013).<br />

(much stronger than either the 2003 or the 2010 heat<br />

waves) are projected to occur as often as every two<br />

years <strong>in</strong> the second half of the 21st century (Map 3.6).<br />

The projected frequency of heat waves is greatest<br />

<strong>in</strong> southern <strong>and</strong> south-eastern <strong>Europe</strong> (Russo et al.,<br />

2014). Accord<strong>in</strong>g to a different analysis, at the end of<br />

the 21st century, 90 % of the summers <strong>in</strong> southern,<br />

central <strong>and</strong> north-western <strong>Europe</strong> will be warmer<br />

than any summer <strong>in</strong> the period 1920–2014 under the<br />

RCP8.5 scenario (Lehner et al., <strong>2016</strong>). The most severe<br />

health risks are projected for low-altitude river bas<strong>in</strong>s<br />

<strong>in</strong> southern <strong>Europe</strong> <strong>and</strong> for the Mediterranean coasts,<br />

where many densely populated urban centres are<br />

located (Fischer <strong>and</strong> Schär, 2010).<br />

78 <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

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!