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90 <strong>Climate</strong> <strong>Change</strong> <strong>and</strong> <strong>Tourism</strong> – Responding to Global Challenges<br />

Large increases in snow-making requirements under climate change scenarios raise questions about the<br />

sustainability <strong>of</strong> this adaptation strategy in certain locations (Box 13). Communities <strong>and</strong> environmental<br />

organizations have expressed concern about the extensive water use <strong>and</strong> chemical additives associated<br />

with snow-making. Even where snow-making is climatically feasible <strong>and</strong> water supplies can be secured,<br />

the additional infrastructure <strong>and</strong> energy costs associated with large increases in snow-making volumes<br />

at higher average temperatures may be uneconomic for some ski operators. Concerns have also been<br />

raised that the increased costs <strong>of</strong> snow-making, particularly for smaller operators at lower elevations,<br />

may again drive skiing to become a ‘sport for the rich’. 456 Regulation <strong>of</strong> the development <strong>and</strong> operation<br />

<strong>of</strong> snow-making systems differs across <strong>and</strong> within nations. In regional ski markets, such as the European<br />

Alps or New Engl<strong>and</strong> states, varied government regulations <strong>and</strong> support for snow-making (through<br />

energy or water subsidies) may provide a competitive advantage to certain ski areas. For example,<br />

chemical-bacterial additives to facilitate snow-making at temperatures near or even above freezing are<br />

allowed in Switzerl<strong>and</strong> 457 , but banned in Germany, <strong>of</strong>fering a competitive edge to Swiss ski areas.<br />

Other important technical adaptation strategies that have been questioned from a sustainability<br />

perspective include glacier preservation <strong>and</strong> expansion <strong>of</strong> ski areas into higher elevations. Glacial<br />

retreat is observed to be a global trend 458 <strong>and</strong> ski areas have utilized two distinct strategies to preserve<br />

glaciers deemed important to their operations. 459 With the increased recession <strong>of</strong> glaciers in the Alps<br />

in recent years, notably the record warm summer <strong>of</strong> 2003, ski areas in Switzerl<strong>and</strong> <strong>and</strong> Austria, have<br />

installed large sheets <strong>of</strong> white polyethylene on critical areas <strong>of</strong> glaciers to protect the ice from ultraviolet<br />

radiation <strong>and</strong> restrict melting during summer months. 460 In Canada, the Whistler-Blackcomb ski resort<br />

is considering an engineering plan to maintain the Horstman Glacier at the top <strong>of</strong> Blackcomb Mountain<br />

by installing snow fences <strong>and</strong> using snow-making near the summit to provide additional snow inputs<br />

for the glacier. 461, 462 The development <strong>of</strong> new skiable terrain at environmentally sensitive higher<br />

elevations, where snow cover is more reliable <strong>and</strong> a longer ski season possible, has also a commonly<br />

identified adaptation strategy. 463, 464, 465 Thirty-six ski areas in Austria applied for permits to exp<strong>and</strong><br />

their operations into higher elevations in 2002–2003. 466<br />

Box 13 The sustainability <strong>of</strong> snow-making<br />

Although concerns have been raised about the environmental impacts <strong>of</strong> snow-making, little<br />

scientific research has been conducted on its differential regional impacts on mountain vegetation,<br />

watersheds or energy use <strong>and</strong> related GHG emissions. Studies have found snow-making to have<br />

a localized affect on ski slope vegetation composition <strong>and</strong> biodiversity <strong>of</strong> high alpine plants by<br />

altering spring soil temperature <strong>and</strong> moisture, as well as the introduction <strong>of</strong> phytopathogenic<br />

bacteria (used as nuclei to enhance ice crystal formulation). 467, 468<br />

Concerns about the tremendous water use by snow-making have largely been focused on the impact<br />

<strong>of</strong> water withdrawals from natural water bodies, <strong>and</strong> there is little knowledge <strong>of</strong> inter-watershed<br />

transfers <strong>of</strong> water or any regional impact on water cycle from snow-making. When water for snowmaking<br />

is withdrawal from natural water bodies (streams <strong>and</strong> lakes), water levels may be reduced<br />

at critical times <strong>of</strong> the year, impacting fish <strong>and</strong> other marine species. Some jurisdictions have<br />

strict regulations governing water withdrawals for snow-making. For example, the State <strong>of</strong> Vermont<br />

(USA) implemented a ‘February Mean Flow’ st<strong>and</strong>ard, where water withdrawals for snow-making<br />

are not permitted when natural watercourses are at or below the average mean flow. To reduce<br />

impacts on natural watercourses, many ski areas have constructed reservoirs to ‘stockpile’ water<br />

during high flow periods (spring freshet) for winter use. No estimates <strong>of</strong> total water withdrawals or<br />

reservoir storage capacity are available for any ski region.<br />

The sustainability <strong>of</strong> snow-making has also been questioned on the basis <strong>of</strong> energy use <strong>and</strong> related<br />

GHG emissions. Snow-making as been referred to as a ‘perverse’ climate change adaptation<br />

because the large projected increase in snow-making under climate change scenarios 469<br />

will further contribute to the very problem <strong>of</strong> adaptation. In tourism, similar arguments could<br />

be made <strong>of</strong> air conditioning in the Mediterranean, Caribbean or other tropical destinations.<br />

UNWTO, 9 July 2008

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