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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 />

Past trends: mean sea level along the <strong>Europe</strong>an<br />

coastl<strong>in</strong>e<br />

Sea level measurements for the <strong>Europe</strong>an region<br />

are available from satellite altimeter observations<br />

(Map 4.3) <strong>and</strong> from tide gauges (Map 4.4). Satellite<br />

observations, which show <strong>change</strong>s <strong>in</strong> absolute sea<br />

level, are available from 1993. Tide gauge records can<br />

be more than 100 years long; they show <strong>change</strong>s <strong>in</strong><br />

relative sea level consider<strong>in</strong>g also l<strong>and</strong> <strong>change</strong>s, which<br />

is more relevant for coastal protection than absolute<br />

sea level. Most <strong>Europe</strong>an coastal regions experience<br />

<strong>in</strong>creases <strong>in</strong> both absolute <strong>and</strong> relative sea level, but<br />

there are sizeable differences between the rates of<br />

absolute <strong>and</strong> relative sea level <strong>change</strong> across <strong>Europe</strong>.<br />

Map 4.3 shows l<strong>in</strong>ear trends <strong>in</strong> absolute sea level<br />

from 1992 to 2014 as observed by satellites. The ma<strong>in</strong><br />

differences between regional seas <strong>and</strong> bas<strong>in</strong>s are<br />

primarily the result of different physical processes<br />

be<strong>in</strong>g the dom<strong>in</strong>ant cause of sea level <strong>change</strong> at<br />

different locations. For <strong>in</strong>stance, the Mediterranean<br />

Sea is a semi-closed, very deep bas<strong>in</strong>, exchang<strong>in</strong>g<br />

water with the Atlantic Ocean through only the<br />

narrow Gibraltar Strait. Sal<strong>in</strong>ity <strong>in</strong> the Mediterranean<br />

Sea may <strong>in</strong>crease <strong>in</strong> the future <strong>and</strong> this will tend to<br />

offset rises <strong>in</strong> sea level due to thermal expansion<br />

from warm<strong>in</strong>g. The NAO, <strong>in</strong>terannual w<strong>in</strong>d variability,<br />

<strong>change</strong>s <strong>in</strong> ocean circulation patterns, <strong>and</strong> the location<br />

of large‐scale gyres <strong>and</strong> small-scale eddies are<br />

further factors that can <strong>in</strong>fluence local sea level <strong>in</strong> the<br />

<strong>Europe</strong>an seas. Obviously, sea level <strong>change</strong>s <strong>in</strong> coastal<br />

zones are most relevant for society.<br />

Map 4.4 shows l<strong>in</strong>ear trends <strong>in</strong> relative sea level from<br />

1970 to 2014 as observed by tide gauge stations <strong>in</strong><br />

<strong>Europe</strong>. These trends can differ from those measured<br />

by satellites because of the longer time period<br />

covered <strong>and</strong> because tide gauge measurements<br />

are <strong>in</strong>fluenced by vertical l<strong>and</strong> movement whereas<br />

satellite measurements are not. In particular, s<strong>in</strong>ce the<br />

last ice age, the l<strong>and</strong>s around the northern Baltic Sea<br />

have been, <strong>and</strong> are still, ris<strong>in</strong>g ow<strong>in</strong>g to the post-glacial<br />

rebound (Johansson et al., 2002).<br />

Map 4.3<br />

Trend <strong>in</strong> absolute sea level across <strong>Europe</strong> based on satellite measurements<br />

-30°<br />

-20°<br />

-10°<br />

0°<br />

10°<br />

20°<br />

30°<br />

40°<br />

50°<br />

60°<br />

70°<br />

Trend <strong>in</strong> absolute sea<br />

level across <strong>Europe</strong><br />

based on satellite<br />

measurements,1992–2014<br />

mm/year<br />

< – 4<br />

60°<br />

– 4 to – 3<br />

– 3 to – 2<br />

50°<br />

– 2 to – 1<br />

– 1 to – 0.5<br />

– 0.5 to 0.5<br />

50°<br />

0.5 to 1<br />

1 to 2<br />

2 to 3<br />

40°<br />

3 to 4<br />

> 4<br />

40°<br />

Outside coverage<br />

0 500 1000 1500 km<br />

0°<br />

10°<br />

20°<br />

30°<br />

40°<br />

Note:<br />

Source:<br />

The map shows the l<strong>in</strong>ear trend <strong>in</strong> sea level <strong>change</strong> over the period 1992–2014. Data uncerta<strong>in</strong>ty is higher along coastal zones than <strong>in</strong><br />

areas further away from the coast. In some regions of the Mediterranean Sea, the depicted trends reflect long-term variability <strong>in</strong> gyres<br />

(i.e. rotat<strong>in</strong>g ocean currents) rather than the effects of climate <strong>change</strong>.<br />

Data supplied by CLS/CNES/LEGOS group (also available through CMEMS).<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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