By Susanne Becken
The e-book offers a finished dialogue of the most recent wisdom within the box of tourism and weather switch. it truly is aimed toward tourism practitioners and people with a tutorial curiosity within the fields of tourism administration and weather swap mitigation, variation and coverage.
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Additional info for Tourism and Climate Change: Risks and Opportunities (Climate Change, Economies and Society)
Since 1850 the glaciers of the European Alps have lost about 30 Á 40% of their surface area and about half of their volume (Beniston, 2003). Paul et al. (2004) report an accelerating loss of glacial ice, with an 18% reduction in area The Tourism Á Climate System 27 between 1985 and 1999. On average the ice masses lost around a third of their surface and half of their volume between the mid-19th century and 1975. Since then, a further 20Á 30% of the ice volume has melted. By 2050 three quarters of today’s Alpine glaciers may well be lost.
This would particularly affect coastal tourism in France, the Netherlands and the UK. 3% of total employment). 8% per annum, in real terms, between 2006 and 2015. Out of 13 regions, the Central and Eastern European travel and tourism economy is ranked fourth regionally in absolute size worldwide, ninth in relative contribution to regional economies and second in long-term (10-year) growth. 2 million) (UNWTO, 2001). Unlike other parts of Europe, maximum warming over Eastern Europe, by about 78C, will occur in winter (Rowell, 2005).
Another important manifestation of the complexities and non-linearities in the climate system is only now being understood, albeit in a preliminary manner. This is the capability of the climate system to undergo abrupt and pervasive changes. Such climate changes have occurred in the past, when the Earth system was forced across thresholds. When this happens, changes in the climate system are no longer controlled by the conditions forcing the change, but by the internal processes of the system. The changes resulting in very different climatic conditions can either be much faster than the forcing (‘abrupt climate change’), or significantly slower, as well as temporary or permanent.