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Climate change impacts and vulnerability in Europe 2016

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<strong>Climate</strong> <strong>change</strong> <strong>impacts</strong> on environmental systems<br />

The bottom panels of Map 4.12 show the comb<strong>in</strong>ed<br />

impact of climate <strong>change</strong> <strong>and</strong> <strong>change</strong>s <strong>in</strong> water<br />

consumption (based on the 'Economy First' water<br />

use scenario) on the same drought <strong>in</strong>dices. In most<br />

regions, projected <strong>in</strong>creases <strong>in</strong> water consumption<br />

further aggravate river flow droughts (Forzieri<br />

et al., 2014, <strong>2016</strong>). Water use <strong>and</strong> abstraction will<br />

exacerbate m<strong>in</strong>imum low-flows <strong>in</strong> many parts of<br />

the Mediterranean region, lead<strong>in</strong>g to <strong>in</strong>creased<br />

probabilities of water deficits when maximum water<br />

dem<strong>and</strong> overlaps with m<strong>in</strong>imum or low availability<br />

(EEA, 2012c).<br />

Map 4.12<br />

Projected <strong>change</strong> <strong>in</strong> 20-year return level m<strong>in</strong>imum flow <strong>and</strong> deficit volumes due to climate<br />

<strong>change</strong> <strong>and</strong> <strong>change</strong>s <strong>in</strong> water use<br />

-30° -20° -10° 0°<br />

M<strong>in</strong>imum discharge<br />

(climate <strong>change</strong> only)<br />

10°<br />

20°<br />

30°<br />

40°<br />

50°<br />

60°<br />

70°<br />

-30° -20° -10° 0°<br />

Deficit volume<br />

(climate <strong>change</strong> only)<br />

10°<br />

20°<br />

30°<br />

40°<br />

50°<br />

60°<br />

70°<br />

60°<br />

60°<br />

50°<br />

50°<br />

50°<br />

50°<br />

40°<br />

40°<br />

40°<br />

40°<br />

0°<br />

10°<br />

20°<br />

30°<br />

40°<br />

0°<br />

10°<br />

20°<br />

30°<br />

40°<br />

-30° -20° -10° 0° 10° 20°<br />

M<strong>in</strong>imum discharge<br />

(climate <strong>change</strong> <strong>and</strong> water use)<br />

30°<br />

40°<br />

50°<br />

60°<br />

70°<br />

-30° -20° -10° 0° 10° 20°<br />

Deficit volume<br />

(climate <strong>change</strong> <strong>and</strong> water use)<br />

30°<br />

40°<br />

50°<br />

60°<br />

70°<br />

60°<br />

60°<br />

50°<br />

50°<br />

50°<br />

50°<br />

40°<br />

40°<br />

40°<br />

40°<br />

0°<br />

10°<br />

20°<br />

30°<br />

40°<br />

0°<br />

10°<br />

20°<br />

30°<br />

40°<br />

Projected <strong>change</strong> <strong>in</strong> 20-year return level m<strong>in</strong>imum flow <strong>and</strong> deficit volumes due to climate <strong>change</strong> <strong>and</strong> <strong>change</strong>s <strong>in</strong> water use<br />

deficits 80 60 40 20 10 5 – 5 – 10 – 20 – 40 – 60 – 80<br />

qm<strong>in</strong><br />

– 80 – 60 – 40 – 20 – 10 – 5 5 10 20 40 60 80<br />

%<br />

Outside coverage<br />

0 500 1 000 1 500 km<br />

Note: This map shows the differences between the end of the 21st century (2071–2100; SRES A1B scenario) <strong>and</strong> the control period (1961–1990)<br />

for m<strong>in</strong>imum flow (left) <strong>and</strong> deficit volume (right) for climate <strong>change</strong> only (top) <strong>and</strong> a comb<strong>in</strong>ation of climate <strong>change</strong> <strong>and</strong> water use<br />

(bottom).<br />

Source: Adapted from Forzieri et al., 2014.<br />

148 <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

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