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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 />

5.6.3 W<strong>in</strong>ter <strong>and</strong> mounta<strong>in</strong> tourism<br />

The w<strong>in</strong>ter sports <strong>in</strong>dustry across <strong>Europe</strong> attracts<br />

millions of tourists each year, generat<strong>in</strong>g nearly<br />

EUR 50 billion <strong>in</strong> annual turnover. The ma<strong>in</strong> w<strong>in</strong>ter sport<br />

dest<strong>in</strong>ation <strong>in</strong> <strong>Europe</strong> is the Alps, where 69 % of Alp<strong>in</strong>e<br />

ski areas <strong>in</strong> Germany, 87 % <strong>in</strong> Austria, 93 % <strong>in</strong> Italy <strong>and</strong><br />

97 % <strong>in</strong> France <strong>and</strong> Switzerl<strong>and</strong> can be considered<br />

as naturally snow reliable under the present climate<br />

(Agrawala, 2007). However, warm w<strong>in</strong>ters have already<br />

affected Alp<strong>in</strong>e w<strong>in</strong>ter tourism. For example, <strong>in</strong> the<br />

record warm w<strong>in</strong>ter of 2006/2007, some low‐altitude<br />

ski areas <strong>in</strong> Austria were not able to offer a cont<strong>in</strong>uous<br />

ski<strong>in</strong>g season from December to April, despite be<strong>in</strong>g<br />

equipped with artificial snow-mak<strong>in</strong>g (Steiger, 2011).<br />

The widespread reductions <strong>in</strong> snow cover projected<br />

over the 21st century will affect snow reliability<br />

<strong>and</strong> consequently the length of the ski season (see<br />

Section 3.3.5). Substantial reductions <strong>in</strong> naturally<br />

snow‐reliable ski areas have been projected for the<br />

Alps, the Pyrenees, the Black Forest region <strong>in</strong> Germany,<br />

<strong>and</strong> Sweden (Agrawala, 2007; Moen <strong>and</strong> Fredman,<br />

2007; Endler <strong>and</strong> Matzarakis, 2011; Steiger <strong>and</strong> Stötter,<br />

2013; Steger et al., 2013; Pons et al., 2015). Low-ly<strong>in</strong>g<br />

ski areas are the most sensitive ski areas to climate<br />

<strong>change</strong>. Studies have estimated that an <strong>in</strong>crease <strong>in</strong><br />

mean temperatures of 1 °C will reduce the ski<strong>in</strong>g season<br />

by four to six weeks <strong>in</strong> low-ly<strong>in</strong>g regions <strong>in</strong> the Alps,<br />

primarily as a result of earlier spr<strong>in</strong>g melt<strong>in</strong>g (Hantel<br />

et al., 2000; Beniston et al., 2003). An analysis for<br />

Switzerl<strong>and</strong> estimates that the altitude limit above which<br />

a region is considered 50 % snow reliable will <strong>in</strong>crease<br />

from 1 400 m <strong>in</strong> the 2000s to 2 200 m <strong>in</strong> the 2080s<br />

under a medium emissions scenario (SRES A1B) (Steger<br />

et al., 2013). Overall, conditions for w<strong>in</strong>ter tourism are<br />

expected to worsen <strong>in</strong> w<strong>in</strong>ter ow<strong>in</strong>g to reduced snow<br />

reliability, with w<strong>in</strong>ter sport activities be<strong>in</strong>g negatively<br />

affected before 2050, particularly at low altitudes <strong>and</strong> <strong>in</strong><br />

the presence of limited adaptation options. On the other<br />

h<strong>and</strong>, traditional w<strong>in</strong>ter sport areas may become more<br />

attractive for tourist activities <strong>in</strong> summer.<br />

Artificial snow-mak<strong>in</strong>g is the ma<strong>in</strong> technical adaptation<br />

option for w<strong>in</strong>ter tourism dest<strong>in</strong>ations. Its cover has<br />

<strong>in</strong>creased significantly <strong>in</strong> recent years, for example<br />

from less than 10 % of the total ski area <strong>in</strong> Switzerl<strong>and</strong><br />

<strong>in</strong> 2000 to 36 % <strong>in</strong> 2010 (Rixen et al., 2011). However,<br />

there are both environmental <strong>and</strong> economic<br />

constra<strong>in</strong>ts to an expansion of artificial snowmak<strong>in</strong>g,<br />

which can offer only limited <strong>and</strong> <strong>in</strong>creas<strong>in</strong>gly<br />

expensive protection from climate <strong>change</strong> <strong>impacts</strong><br />

(Steiger <strong>and</strong> Stötter, 2013; Damm et al., 2014; Kovats<br />

et al., 2014). Investments <strong>in</strong> alternative activities<br />

dur<strong>in</strong>g w<strong>in</strong>ter or all-year-round tourism may partly<br />

compensate for the loss <strong>in</strong> overnight stays, depend<strong>in</strong>g<br />

on the attractiveness of the location for non-w<strong>in</strong>ter<br />

sport tourism.<br />

The economic impact of the worsen<strong>in</strong>g snow reliability<br />

projected for most <strong>Europe</strong>an ski resorts depends<br />

strongly on tourists' adaptation choices. When tourists<br />

stick to ski<strong>in</strong>g but <strong>change</strong> the month (with<strong>in</strong> the w<strong>in</strong>ter<br />

season) <strong>in</strong> which they go <strong>and</strong>/or the dest<strong>in</strong>ation, this<br />

will affect the competition between ski<strong>in</strong>g areas, with<br />

the southern part of the Alps (e.g. <strong>in</strong> France <strong>and</strong> Italy)<br />

los<strong>in</strong>g overnight stays <strong>and</strong> the comparatively snowreliable<br />

northern parts of the Alps <strong>and</strong> Sc<strong>and</strong><strong>in</strong>avia<br />

benefitt<strong>in</strong>g from climate <strong>change</strong>. If tourists <strong>change</strong><br />

their holiday type, all ski<strong>in</strong>g areas face a reduction <strong>in</strong><br />

overnight stays (Perrels et al., 2015).<br />

Socio-economic <strong>and</strong> demographic <strong>change</strong>s can also be<br />

important factors for future w<strong>in</strong>ter sport tourism. One<br />

study on the Austrian Alps concluded that decl<strong>in</strong><strong>in</strong>g<br />

<strong>and</strong>/or age<strong>in</strong>g populations <strong>in</strong> source countries are a<br />

more immediate threat than climate <strong>change</strong> to w<strong>in</strong>ter<br />

tourism <strong>in</strong> the first half of the 21st century, after which<br />

the effect of ris<strong>in</strong>g temperatures will dom<strong>in</strong>ate (Steiger,<br />

2012).<br />

Some w<strong>in</strong>ter tourism, <strong>in</strong> particular <strong>in</strong> Nordic regions,<br />

depends on a snowy l<strong>and</strong>scape, despite not necessarily<br />

be<strong>in</strong>g related to w<strong>in</strong>ter sport activities. Hence, Nordic<br />

tourism can be threatened by the loss of reliable snow<br />

cover <strong>in</strong> w<strong>in</strong>ter <strong>and</strong> the related damage to the general<br />

perceptions of the northern l<strong>and</strong>scape as a snowcovered<br />

backdrop of outdoor <strong>and</strong> traditional activities,<br />

even outside w<strong>in</strong>ter sport resorts (Tervo-Kankare et al.,<br />

2013; Kaján, 2014).<br />

266 <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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