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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 society<br />

5.4 Energy<br />

Key messages<br />

• <strong>Climate</strong> <strong>change</strong> has affected the dem<strong>and</strong> for heat<strong>in</strong>g <strong>and</strong> will affect future energy dem<strong>and</strong> more generally. The total<br />

energy dem<strong>and</strong> <strong>in</strong> <strong>Europe</strong> is not expected to <strong>change</strong> substantially, but significant seasonal shifts <strong>and</strong> effects on the energy<br />

mix are expected, with large regional differences.<br />

• The number of population-weighted heat<strong>in</strong>g degree days has decreased <strong>in</strong> recent decades, whereas the number of<br />

cool<strong>in</strong>g degree days has <strong>in</strong>creased. As a result, the energy dem<strong>and</strong> for heat<strong>in</strong>g has decreased, particularly <strong>in</strong> northern<br />

<strong>and</strong> north-western <strong>Europe</strong>, whereas the energy dem<strong>and</strong> for cool<strong>in</strong>g has <strong>in</strong>creased, <strong>in</strong> particular <strong>in</strong> southern <strong>and</strong> central<br />

<strong>Europe</strong>. The absolute <strong>change</strong> is larger for heat<strong>in</strong>g degree days, but the relative <strong>change</strong> is larger for cool<strong>in</strong>g degree days.<br />

• Further <strong>in</strong>creases <strong>in</strong> temperature <strong>and</strong> the occurrence of droughts may limit the availability of cool<strong>in</strong>g water for thermal<br />

power generation <strong>in</strong> summer when the abundance of cool<strong>in</strong>g water is at its lowest.<br />

• Increas<strong>in</strong>g temperatures, chang<strong>in</strong>g precipitation patterns <strong>and</strong> possible <strong>in</strong>creases <strong>in</strong> storm severity <strong>and</strong> frequency can have<br />

an impact on both renewable <strong>and</strong> conventional electricity generators. Most of the projected <strong>impacts</strong> of climate <strong>change</strong><br />

will be negative, but some positive <strong>impacts</strong> may occur, <strong>in</strong> particular for renewable energy production <strong>in</strong> northern <strong>Europe</strong>.<br />

• Energy transport <strong>in</strong>frastructures across <strong>Europe</strong> are exposed to substantial risks from <strong>in</strong>creas<strong>in</strong>g frequency <strong>and</strong> magnitude<br />

of extreme events <strong>in</strong>duced by climate <strong>change</strong>. Infrastructures <strong>in</strong> mounta<strong>in</strong> regions will be threatened by geological<br />

<strong>in</strong>stability ow<strong>in</strong>g to <strong>in</strong>creased precipitation. Countries <strong>in</strong> north-western <strong>Europe</strong> appear to be ahead <strong>in</strong> preparedness<br />

regard<strong>in</strong>g coastal energy <strong>in</strong>frastructure.<br />

5.4.1 Overview<br />

Relevance<br />

Energy plays a fundamental role <strong>in</strong> support<strong>in</strong>g all<br />

aspects of modern life. This sector is responsible<br />

directly or <strong>in</strong>directly for the majority of anthropogenic<br />

greenhouse gas emissions (Edenhofer et al., 2014).<br />

At the same time, both energy supply <strong>and</strong> energy<br />

dem<strong>and</strong> are sensitive to <strong>change</strong>s <strong>in</strong> climate, <strong>in</strong><br />

particular <strong>in</strong> temperature. The <strong>in</strong>creas<strong>in</strong>g frequency<br />

of extreme weather events, <strong>in</strong>clud<strong>in</strong>g heat waves,<br />

droughts <strong>and</strong> potentially storms, poses additional<br />

challenges for energy systems (Rademaekers et al.,<br />

2011). In particular, the efficiency <strong>and</strong> outputs of<br />

thermal power plants can be adversely affected by a<br />

rise <strong>in</strong> temperature or a decrease <strong>in</strong> the availability<br />

of cool<strong>in</strong>g water (low flows as a result of droughts).<br />

Storms, extreme w<strong>in</strong>d gusts <strong>and</strong> ice storms could<br />

also pose a challenge for energy <strong>in</strong>frastructure, such<br />

as transmission <strong>and</strong> distribution networks, as well<br />

as renewable generators. Increased flood<strong>in</strong>g could<br />

affect power stations <strong>and</strong> substations. Changed<br />

precipitation patterns or variability could create<br />

greater uncerta<strong>in</strong>ty when <strong>in</strong>vest<strong>in</strong>g <strong>in</strong> hydropower<br />

facilities <strong>and</strong> could alter output, but could also result<br />

<strong>in</strong> local benefits from <strong>in</strong>creased hydropower output<br />

<strong>in</strong> some regions. Hydropower production could also<br />

be affected by <strong>in</strong>creased silt<strong>in</strong>g of sediment <strong>in</strong>to<br />

reservoirs caused by <strong>in</strong>creased erosion <strong>and</strong> sediment<br />

displacement as a consequence of climate <strong>change</strong>.<br />

Other renewable energy supplies could also be affected<br />

by climate <strong>change</strong>, <strong>in</strong> particular through <strong>impacts</strong> on the<br />

production of bioenergy, but also on w<strong>in</strong>d turb<strong>in</strong>es <strong>and</strong><br />

solar cells.<br />

<strong>Climate</strong> <strong>change</strong> is reduc<strong>in</strong>g the dem<strong>and</strong> for space<br />

heat<strong>in</strong>g <strong>and</strong> <strong>in</strong>creas<strong>in</strong>g the dem<strong>and</strong> for space cool<strong>in</strong>g,<br />

both globally <strong>and</strong> <strong>in</strong> <strong>Europe</strong>. However, socio-economic<br />

<strong>and</strong> technical factors also play an important role <strong>in</strong><br />

the future energy dem<strong>and</strong> for heat<strong>in</strong>g <strong>and</strong> cool<strong>in</strong>g.<br />

Projected <strong>in</strong>creases <strong>in</strong> <strong>in</strong>come levels <strong>in</strong> the EU are<br />

considered the ma<strong>in</strong> driver for <strong>in</strong>creases <strong>in</strong> the cool<strong>in</strong>g<br />

dem<strong>and</strong> up to 2050, while energy efficiency upgrades<br />

<strong>and</strong> dem<strong>and</strong>-side management are curb<strong>in</strong>g future<br />

energy dem<strong>and</strong>. This latter factor is particularly<br />

relevant to the fact that the energy sector is a major<br />

source of greenhouse gas emissions <strong>and</strong>, therefore,<br />

is a major target of mitigation policies. Modell<strong>in</strong>g<br />

the possible future <strong>impacts</strong> of climate <strong>change</strong> on<br />

energy dem<strong>and</strong> requires alternative scenarios to be<br />

modelled, which typically differ <strong>in</strong> the strength of<br />

the mitigation policies to be adopted, which <strong>in</strong> turn<br />

may support energy efficiency <strong>and</strong> thus contribute to<br />

reduc<strong>in</strong>g energy dem<strong>and</strong>, or may modify the energy<br />

mix <strong>and</strong> therefore the exposure of the energy system<br />

to stresses <strong>in</strong>duced by climate <strong>change</strong> such as water<br />

scarcity (Dowl<strong>in</strong>g, 2013; Mima <strong>and</strong> Criqui, 2015).<br />

244 <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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