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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 />

4.3.5 Water temperature<br />

Key messages<br />

• Water temperatures <strong>in</strong> major <strong>Europe</strong>an rivers have <strong>in</strong>creased by 1–3 °C over the last century. Several time series show<br />

<strong>in</strong>creas<strong>in</strong>g lake <strong>and</strong> river temperatures all over <strong>Europe</strong> s<strong>in</strong>ce the early 1900s.<br />

• Lake <strong>and</strong> river surface water temperatures are projected to <strong>in</strong>crease further with projected <strong>in</strong>creases <strong>in</strong> air temperature.<br />

• Increased water temperature can result <strong>in</strong> marked <strong>change</strong>s <strong>in</strong> species composition <strong>and</strong> function<strong>in</strong>g of aquatic ecosystems.<br />

Relevance<br />

Water temperature is one of the parameters that<br />

determ<strong>in</strong>e the overall health of aquatic ecosystems.<br />

Most aquatic organisms have a specific range of<br />

temperatures that they can tolerate, which determ<strong>in</strong>es<br />

their spatial distribution. Changes <strong>in</strong> temperature also<br />

determ<strong>in</strong>e ice cover periods, thermal stratification of<br />

lakes, nutrient availability <strong>and</strong> the duration of grow<strong>in</strong>g<br />

seasons that <strong>in</strong> turn affect species composition <strong>and</strong><br />

food web structures (e.g. Moss et al., 2009; Markovic<br />

et al., 2014).<br />

Past trends<br />

The surface water temperatures of major rivers <strong>in</strong><br />

<strong>Europe</strong> have <strong>in</strong>creased by 1–3 °C over the last century<br />

(Figure 4.14). For example, the average temperature<br />

<strong>in</strong> the Rh<strong>in</strong>e near Basel, Switzerl<strong>and</strong>, has risen by<br />

more than 2 °C s<strong>in</strong>ce the 1960s (FOEN, 2015). The<br />

temperature of the downstream part of the Rh<strong>in</strong>e<br />

<strong>in</strong>creased by nearly 3 °C between 1910 <strong>and</strong> 2013.<br />

A similar <strong>in</strong>crease of 2.4 °C has been observed <strong>in</strong> the<br />

Meuse. Two-thirds of the <strong>in</strong>crease of the downstream<br />

part of the Rh<strong>in</strong>e is attributed to the <strong>in</strong>creased use of<br />

Figure 4.14<br />

Observed trends <strong>in</strong> water temperature of large <strong>Europe</strong>an rivers <strong>and</strong> lakes<br />

Degrees celcius (°C)<br />

25<br />

20<br />

15<br />

10<br />

5<br />

0<br />

1900 1920 1940 1960 1980 2000<br />

Rh<strong>in</strong>e, Lobith<br />

Meuse, Eijsden<br />

Lake Võrtsjärv, Estonia<br />

Danube, Vienna<br />

Lake Saimaa, F<strong>in</strong>l<strong>and</strong><br />

Note:<br />

This figure shows the annual average water temperature <strong>in</strong> the Rh<strong>in</strong>e <strong>and</strong> the Meuse (1911–2013), the Danube (1901–1998) <strong>and</strong> Lake<br />

Võrtsjärv (1947–2014), <strong>and</strong> the average water temperature <strong>in</strong> August <strong>in</strong> Lake Saimaa, F<strong>in</strong>l<strong>and</strong> (1924–2014).<br />

Source: Rh<strong>in</strong>e <strong>and</strong> Meuse (CBS et al., 2014); Danube (Hohens<strong>in</strong>ner, 2006, personal communication); Lake Saimaa (Johanne Korhonen, 2015,<br />

personal communication); Lake Võrtsjärv (Peeter Nõges, 2015, personal communication).<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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