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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 />

4.1 Oceans <strong>and</strong> mar<strong>in</strong>e environment<br />

Key messages<br />

• The primary <strong>impacts</strong> of climate <strong>change</strong> observed <strong>in</strong> <strong>Europe</strong>'s seas are acidification, <strong>in</strong>creased ocean heat content <strong>and</strong><br />

<strong>in</strong>creased sea surface temperature. The extent to which physical <strong>impacts</strong> have been documented varies among the seas.<br />

• <strong>Climate</strong> <strong>change</strong> affects physical conditions differently <strong>in</strong> <strong>Europe</strong>'s seas, <strong>and</strong> consequently its biological <strong>impacts</strong> also vary<br />

depend<strong>in</strong>g on the region. Ocean temperature is one of the strongest regulators of mar<strong>in</strong>e life. Changes <strong>in</strong> temperature<br />

cause significant shifts <strong>in</strong> the distribution of mar<strong>in</strong>e species, both horizontally, towards the poles, <strong>and</strong> vertically, with<br />

<strong>change</strong>s <strong>in</strong> depth distribution.<br />

• The <strong>impacts</strong> of climate <strong>change</strong> <strong>in</strong> comb<strong>in</strong>ation with synergistic <strong>impacts</strong> of other anthropogenic stressors will potentially<br />

cause widespread <strong>change</strong>s to mar<strong>in</strong>e ecosystems <strong>and</strong> ultimately the services <strong>and</strong> benefitss humans receive from the seas.<br />

• North-east Atlantic Ocean: sea surface temperature <strong>and</strong> ocean heat content are <strong>in</strong>creas<strong>in</strong>g <strong>in</strong> all regions, although<br />

at different rates. Sea surface temperature <strong>change</strong>s have already resulted <strong>in</strong> an <strong>in</strong>creased duration of the mar<strong>in</strong>e<br />

grow<strong>in</strong>g season <strong>and</strong> <strong>in</strong> the northwards movement of mar<strong>in</strong>e zooplankton. Mar<strong>in</strong>e species are shift<strong>in</strong>g their distributions<br />

northwards <strong>in</strong> response to <strong>in</strong>creased temperatures. Of the commonly observed demersal fish species, 72 % have<br />

experienced <strong>change</strong>s <strong>in</strong> abundance <strong>and</strong>/or distribution <strong>in</strong> response to warm<strong>in</strong>g waters. This <strong>change</strong> has already had<br />

important <strong>impacts</strong> on fisheries <strong>in</strong> this region.<br />

• Baltic Sea: future climate <strong>change</strong> is projected to warm the Baltic Sea, to decrease its sal<strong>in</strong>ity, to decrease sea ice extent by<br />

50–80 % dur<strong>in</strong>g the 21st century, <strong>and</strong> to further exp<strong>and</strong> oxygen depleted 'dead zones'. These <strong>change</strong>s <strong>in</strong> physical variables<br />

will have predom<strong>in</strong>antly negative <strong>impacts</strong> on the Baltic Sea ecosystems.<br />

• Mediterranean Sea: temperature is projected to <strong>in</strong>crease, <strong>and</strong> run-off to the Mediterranean Sea is projected to decrease,<br />

thereby <strong>in</strong>creas<strong>in</strong>g sal<strong>in</strong>ity. Stratification is projected to rema<strong>in</strong> largely constant because of the compensat<strong>in</strong>g effects of<br />

<strong>in</strong>creas<strong>in</strong>g temperature <strong>and</strong> <strong>in</strong>creas<strong>in</strong>g sal<strong>in</strong>ity on the density of sea water. The observed <strong>in</strong>vasion <strong>and</strong> survival of alien<br />

species has been correlated with the warm<strong>in</strong>g trend <strong>in</strong> sea surface temperature.<br />

4.1.1 Overview<br />

Relevance<br />

The oceans cover about 72 % of the Earth's surface.<br />

Oceans <strong>in</strong>teract closely with the atmosphere. On the<br />

one h<strong>and</strong>, oceans <strong>in</strong>fluence weather patterns on local<br />

to global scales. On the other h<strong>and</strong>, <strong>change</strong>s <strong>in</strong> the<br />

atmosphere can alter the properties of the oceans.<br />

Changes <strong>in</strong> ocean properties driven by an <strong>in</strong>crease<br />

<strong>in</strong> atmospheric greenhouse gas concentrations,<br />

such as ocean acidification <strong>and</strong> warm<strong>in</strong>g, can have<br />

a substantial impact on mar<strong>in</strong>e ecosystems, their<br />

productivity <strong>and</strong> mar<strong>in</strong>e biodiversity, <strong>and</strong> thus<br />

ecosystem-service provision (Walther et al., 2002;<br />

Lotze et al., 2006; Ruckelshaus et al., 2013).<br />

The atmospheric concentrations of greenhouse<br />

gases, such as CO 2 , have <strong>in</strong>creased substantially s<strong>in</strong>ce<br />

pre‐<strong>in</strong>dustrial times, thus trapp<strong>in</strong>g <strong>in</strong>creas<strong>in</strong>gly more<br />

solar energy with<strong>in</strong> the atmosphere (see Section 3.1).<br />

Most of this heat is stored by the ocean, where it<br />

affects sea surface temperature, ocean heat content,<br />

sea levels, sal<strong>in</strong>ity, ocean circulation <strong>and</strong> sea ice<br />

cover. The rest melts ice <strong>and</strong> warms the atmosphere<br />

<strong>and</strong> l<strong>and</strong>. The ocean also absorbs significant amounts<br />

of CO 2 from the atmosphere, thereby mitigat<strong>in</strong>g the<br />

magnitude of climate <strong>change</strong>. However, the <strong>in</strong>creased<br />

levels of dissolved carbon are chang<strong>in</strong>g the chemistry<br />

of seawater <strong>and</strong> mak<strong>in</strong>g it more acidic. Sea level rise<br />

is addressed <strong>in</strong> Section 4.2.<br />

Changes to the physical <strong>and</strong> chemical properties of<br />

the ocean can have substantial <strong>impacts</strong> on mar<strong>in</strong>e<br />

biodiversity <strong>and</strong> thus alter mar<strong>in</strong>e ecosystem<br />

productivity, function<strong>in</strong>g <strong>and</strong> ecosystem-service<br />

provision. As such, climate <strong>change</strong> affects the<br />

health <strong>and</strong> resilience of mar<strong>in</strong>e ecosystems <strong>and</strong> the<br />

provision of services to society, such as through<br />

fisheries. These effects of climate <strong>change</strong> are now<br />

be<strong>in</strong>g seen <strong>in</strong> all of <strong>Europe</strong>'s seas, although the<br />

extent to which <strong>impacts</strong> have been documented<br />

106 <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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