Climate Change and Tourism - UNEP - Division of Technology ...
Climate Change and Tourism - UNEP - Division of Technology ...
Climate Change and Tourism - UNEP - Division of Technology ...
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UNWTO, 9 July 2008<br />
Impacts <strong>and</strong> Adaptation at <strong>Tourism</strong> Destinations<br />
Critically, the heavily cited OECD analysis did not account for snow-making. It therefore does not<br />
reflect the operating realities <strong>of</strong> many ski operators <strong>and</strong> has likely overestimated the potential damages<br />
to these businesses. Major uncertainties on the impacts for businesses also relate to the acceptance <strong>of</strong><br />
customers to ski on partially snow covered ski runs, such as illustrated in Figure 9.2, or the potential for<br />
large reductions in opportunities for Nordic skiing at low mountain elevations.<br />
The winter <strong>of</strong> 2006-2007 was the warmest on record over most parts <strong>of</strong> the Alps <strong>and</strong> estimated to be the<br />
warmest winter in the past millennium in some locations. 284, 285 The impact <strong>of</strong> this record warm winter<br />
on the ski industry is still being tabulated, but the delayed opening <strong>of</strong> the season <strong>and</strong> inability to make<br />
snow in some locations were prominent impacts. Analysis <strong>of</strong> this climate change analogue will provide<br />
important new information on the ability <strong>of</strong> ski areas to operate <strong>and</strong> remain pr<strong>of</strong>itable under conditions<br />
similar to those projected decades from now.<br />
Figure 9.2 Partially operating ski area near Salzburg, Austria (mid-January 2007)<br />
Scotl<strong>and</strong><br />
Photo credit: Stadel, B.<br />
Trends in ski season length at the Cairngorm ski area in Scotl<strong>and</strong> from 1972 to 1996 reveal a shorter<br />
average season, but at the highest elevation ski lift (1,060–1,150 m) there was no change. 286 Based on<br />
an analysis <strong>of</strong> the exceptionally mild winter <strong>of</strong> 1988–1989, it has been suggested that ski areas above<br />
1,000 m would still have sufficient natural snow cover for skiing in warmer winters. 287 However, the<br />
warm winter <strong>of</strong> 1988–1989 was not compared against future climate change scenarios for this region,<br />
so the future operation <strong>of</strong> ski areas in Scotl<strong>and</strong> remains uncertain.<br />
Eastern North America<br />
Snow-making is integral to the ski industry in Eastern Canada <strong>and</strong> the US <strong>and</strong> most ski areas have<br />
virtually complete coverage <strong>of</strong> their skiable terrain. A second generation <strong>of</strong> climate change assessments,<br />
which account for snow-making, have substantially improved our underst<strong>and</strong>ing <strong>of</strong> the risk climate<br />
change poses to the ski industry in this region. 288, 289 Advanced snow-making systems substantially<br />
lower the vulnerability <strong>of</strong> ski areas in eastern North America to climate change at least through the<br />
middle <strong>of</strong> the 21st century. Ski season losses are projected to range from 8–46% in Ontario <strong>and</strong> 4–34%<br />
in Quebec depending on the climate change scenario, with high emission scenarios causing much larger<br />
impacts. 290, 291 In New Engl<strong>and</strong>, with advanced snow-making capabilities, only one <strong>of</strong> 14 locations<br />
was projected to lose greater than 25% <strong>of</strong> its ski season under low emission scenarios by mid century.<br />
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