Climatic Change

, Volume 119, Issue 3–4, pp 965–978 | Cite as

A comparative assessment of the potential impact of climate change on the ski industry in New Zealand and Australia

  • J. Hendrikx
  • C. Zammit
  • E. Ö. Hreinsson
  • S. Becken
Article

Abstract

In this paper we assess the impact of climate change, at a micro-scale for a selection of four sites in New Zealand and Australia. These sites are representative of the key destination ski regions. In contrast to previous work, our work will for the first time, allow for a direct comparison between these two countries and enable both an estimate of the absolute impacts at a given site, as well as the relative impacts between the two countries. This direct comparison is possible because we have used exactly the same snow model, the same 3 global climate models (GCMs) and the same techniques to calibrate the model for all locations. We consider the changes in natural snow at these locations for the 2030–2049 and 2080–2099 time periods, for one mid-range emissions scenario (A1B). This future scenario is compared to simulations of current, 1980–1999, snow at these locations. We did not consider the snowmaking or economic components of the ski industry vulnerability, only the modelled changes in the natural snow component. At our New Zealand sites, our model indicates that by the 2040s there will be on average between 90 % and 102 % of the current maximum snow depth (on 31 August) and by the 2090s this will be on average reduced to between 46 % and 74 %. In Australia, our models estimates that by the 2040s there will be on average between 57 % and 78 % of the current maximum snow depth and by the 2090s this will be on average further reduced to between 21 % and 29 %. In terms of days with snowdepths equal to or exceeding a ski industry useable levels of 0.30 m, at our lowest elevation, and most sensitive sites, we observe a change from 125 days (current) to 99–126 (2040s) and 52–110 (2090s) in New Zealand. In Australia, a reduction from 94 to 155 days (current) to 81–114 (2040s) and 0–75 (2090s) is observed. In each case the changes are highly depended on the GCM used to drive the climate change scenario. While the absolute changes will have direct impacts at each location, so too will the relative changes with respect to future potential Australia–New Zealand tourism flows, and beyond. Our study provides an approach by which other regions or countries with climate sensitive tourism enterprises could assess the relative impacts and therefore the potential wider ranging ramifications with respect to destination attractiveness.

References

  1. Abegg B, Agrawala S, Crick F, de Montfalcon A (2007) Climate change impacts and adaptation in winter tourism. In: Climate change in the European Alps: adapting winter tourism and natural hazards management. Paris: Organization for Economic Co-operation and Development, pp 25−60Google Scholar
  2. Becken S, Hay J (2012) Tourism and climate change—from policy to practice. Routledge, LondonGoogle Scholar
  3. Beniston M, Uhlmann B, Goyettea S, Lopez-Morenob JI (2011) Will snow-abundant winters still exist in the Swiss Alps in an enhanced greenhouse climate? Inte J Climatol 31(9):1257–1263CrossRefGoogle Scholar
  4. Bicknell S, McManus P (2006) The canary in the coalmine: Australian ski resorts and their response to climate change. Geogr Res 44:386–400CrossRefGoogle Scholar
  5. Clark MP, Slater AG (2006) Probabilistic quantitative precipitation estimation in complex terrain. J Hydrometeorol 7(1):3–22CrossRefGoogle Scholar
  6. Clark M, Örn Hreinsson E, Martinez G, Tait A, Slater A, Hendrikx J, Owens I, Gupta H, Schmidt J, Woods R (2009) Simulations of seasonal snow for the South Island, New Zealand. J Hydrol (NZ) 48(2):41–58Google Scholar
  7. CSIRO and BoM (2007) Climate change in Australia. Technical Report by CSIRO and the Australian Bureau of Meteorology, 150 pp, www.climatechangeinaustralia.gov.au
  8. Dawson J, Scott D, McBoyle G (2009) Climate change analogue analysis of ski tourism in the northeastern USA. Clim Res 39:1–9CrossRefGoogle Scholar
  9. Elsasser H, Messerli P (2001) The vulnerability of the snow industry in the Swiss Alps. Mt Res Dev 21(4):335–339CrossRefGoogle Scholar
  10. Fukushima T, Kureha M, Ozaki N et al (2003) Influences of air temperature change on leisure industries: case study on ski activities. Mitig Adapt Strateg Clim Chang 7:173–189CrossRefGoogle Scholar
  11. Hayhoe K, Cayan D, Field C et al (2004) Emission pathways, climate change, and impacts on California. Proc Natl Acad Sci 101(34):12422–12427CrossRefGoogle Scholar
  12. Hennessy KJ, Whetton PH, Bathols J, Hutchinson M, Sharples J (2003) The impact of climate change on snow conditions in Australia. Consultancy report for the Victorian Dept of Sustainability and Environment, NSW National Parks and Wildlife Service, Australian Greenhouse Office and the Australian Ski Areas Association., CSIRO Atmospheric Research, 47 pp http://www.cmar.csiro.au/e-print/open/hennessy_2003a.pdf
  13. Hennessy KL, Whetton PH, Walsh K, Smith IN, Bathols JM, Hutchinson M, Sharples J (2008) Climate change effects on snow conditions in mainland Australia and adaptation at ski resorts through snow making. Clim Res 35:255–270CrossRefGoogle Scholar
  14. Hendrikx J, Hreinsson EÖ (2012) The potential impact of climate change on seasonal snow in New Zealand: part II—industry vulnerability and future snowmaking potential. Theor Appl Climatol 110(4):619–630. doi:10.1007/s00704-012-0713-z CrossRefGoogle Scholar
  15. Hendrikx J, Hreinsson EÖ, Clark MP, Mullan AB (2012) The potential impact of climate change on seasonal snow in New Zealand: part I—an analysis using 12 GCMs. Theor Appl Climatol 110(4):607–618. doi:10.1007/s00704-012-0711-1 CrossRefGoogle Scholar
  16. Hopkins D, Becken S, Hendrikx J (2011) Australian snow tourist’s perceptions of climate change: implications for the Queenstown Lakes region of New Zealand. In: Borsdorf A, Stötter J, Veulliet E (eds) 2011: Managing Alpine Future II—inspire and drive sustainable mountain regions. Proceedings of the Innsbruck Conference, November 21–23, 2011. (= IGF-Forschungsberichte 4). Verlag der Österreichischen Akademie der Wissenschaften: WienGoogle Scholar
  17. Hopkins D, Higham JES, Becken S (2012) Climate change in a regional context: relative vulnerability in the Australasian skier market. Reg Environ Chang. doi:10.1007/s10113-012-0352-z Google Scholar
  18. Hoy A, Hänsel S, Matschullat J (2011) How can winter tourism adapt to climate change in Saxony’s mountains? Reg Environ Chang 11(3):459–469CrossRefGoogle Scholar
  19. Hutchinson MF (1998a) Interpolation of rainfall data with thin plate smoothing splines—part I: two dimensional smoothing of data with short range correlation. J Geogr Inf Decis Anal 2(2):139–151Google Scholar
  20. Hutchinson MF (1998b) Interpolation of rainfall data with thin plate smoothing splines—part II: analysis of topographic dependence. J Geogr Inf Decis Anal 2(2):152–167Google Scholar
  21. Irving DB, Perkins SE, Brown JR, Sen Gupta A et al (2011) Evaluating global climate models for the Pacific island region. Clim Res 49:169–187CrossRefGoogle Scholar
  22. Ministry for the Environment (MfE) (2008) Climate change effects and impacts assessment. A guidance manual for local government in New Zealand. 2nd edn. Prepared by Mullan B, Wratt D, Dean S, Hollis M (NIWA), Allan S, Williams T (MWH NZ Ltd), Kenny G (Earthwise Consulting Ltd), in consultation with MfE. NIWA Client Report No. WLG2007/62. 156 pGoogle Scholar
  23. Ministry for the Environment (MfE) (2010) Tools for estimating the effects of climate change on flood flow: A guidance manual for local government in New Zealand. Prepared by Woods R, Mullan AB, Smart G, Rouse H, Hollis M, McKerchar A, Ibbitt R, Dean S, Collins D (NIWA). Prepared for MfE. 63 p. NIWA Client Report. [available on line at http://www.mfe.govt.nz/publications/climate/climate-change-effects-on-flood-flow/index.html]
  24. Moen J, Fredman P (2007) Effects of climate change on alpine skiing in Sweden. J Sustain Tour 15:418–437CrossRefGoogle Scholar
  25. Peters GP, Andrew RM, Boden T, Canadell JG, Ciais P, Le Quere C, Marland G, Raupach MR, Wilson C (2012) The challenge to keep global warming below 2°C. Nat Clim Chang. doi:10.1038/nclimate1783 Google Scholar
  26. Pickering CM, Buckley RC (2010) Climate response by the ski industry: the shortcomings of snowmaking for Australian resorts. AMBIO: J Hum Environ 39(5–6):430–438CrossRefGoogle Scholar
  27. Pickering CM, Castley JG, Burtt M (2009) Skiing less often in a warmer world: attitudes of tourists to climate change in an Australian ski resort. Geogr Res 48(2):137–147CrossRefGoogle Scholar
  28. Rixen C, Teich M, Lardelli C, Gallati D, Pohl M, Pütz M, Bebi P (2011) Winter tourism and climate change in the Alps: an assessment of resource consumption, snow reliability and future snowmaking potential. Mt Res Dev 31(3):229–236CrossRefGoogle Scholar
  29. Scherrer SC, Appenzeller C, Laternser M (2004) Trends in Swiss Alpine snow days: the role of local- and large-scale variability. Geophys Res Lett 31(L13215):1–4Google Scholar
  30. Scott D, McBoyle G, Minogue A (2007) Climate change and Quebec’s ski industry. Glob Environ Chang 17:181–190CrossRefGoogle Scholar
  31. Scott D, Dawson J, Jones B (2011) Climate change vulnerability of the US Northeast winter recreation—tourism sector. Mitig Adapt Strateg Glob Chang 13(5–6):577–596Google Scholar
  32. Shih C, Nicholls S, Holecek D (2009) Impact of weather on Downhill ski lift ticket sales. J Travel Res 47(3):359–372CrossRefGoogle Scholar
  33. Steiger R (2010) The impact of climate change on ski season length and snowmaking requirements in Tyrol, Austria. Clim Res 43:251–262CrossRefGoogle Scholar
  34. Suppiah R, Hennessy KJ, Whetton PH, McInnes K, Macadam I, Bathols J, Ricketts J, Page CM (2007) Australian climate change projections derived from simulations performed for the IPCC 4th Assessment Report. Aust Meteorol Mag 56(2007):131–152Google Scholar
  35. Tait AB (2008) Future projections of growing degree days and frost in New Zealand and some implications for grape growing. Weather Clim 28:17–36Google Scholar
  36. Tait A, Henderson RD, Turner R, Zheng X (2006) Thin plate smoothing spline interpolation of daily rainfall for New Zealand using a climatological rainfall surface. Int J Climatol 26(14):2097–2115CrossRefGoogle Scholar
  37. The National Climate Database (2013) (CliFlo). NIWA. http://cliflo.niwa.co.nz/ [Accessed 02 January, 2013]
  38. Woods R, Hendrikx J, Henderson R, Tait A (2006) Estimating mean flow of New Zealand rivers. J Hydrol (NZ) 45(2):95–110Google Scholar

Copyright information

© Springer Science+Business Media Dordrecht 2013

Authors and Affiliations

  • J. Hendrikx
    • 1
  • C. Zammit
    • 2
  • E. Ö. Hreinsson
    • 2
  • S. Becken
    • 3
  1. 1.Snow and Avalanche Laboratory, Department of Earth SciencesMontana State UniversityBozemanUSA
  2. 2.National Institute of Water and Atmospheric Research (NIWA)ChristchurchNew Zealand
  3. 3.Department of Tourism, Leisure, Hotel & Sport MgtGriffith UniversitySouthportAustralia

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