Abstract
Alpine regions have been and will be responding sensitively to global climate change compared to other European regions. This chapter analyses past and future changes in the climate of the Alps and its consequences on the elements of the water cycle. One obvious consequence is the melting of European glaciers by more than 65% since the end of the Little Ice Age in 1850. As a result of temperature increase hydrological regimes are changing. How will climate and water balance change in the future? Scenario results for the European Alps and in more detail for the Swiss Alps are discussed. Consequences in inner Alpine valleys are less precipitation in summer and hence more droughts.
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Acknowledgments
The authors wish to thank Alexander Hermann for excellent support in preparing all figures of this chapter.
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Schädler, B., Weingartner, R. (2010). Impact of Climate Change on Water Resources in the Alpine Regions of Switzerland. In: Bundi, U. (eds) Alpine Waters. The Handbook of Environmental Chemistry(), vol 6. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-88275-6_3
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