Localized climate change scenarios of mean temperature and precipitation over Switzerland

• Published in: Climatic change 2014-07, Vol.125 (2), p.237-252
• Main Authors: Zubler, Elias M., Fischer, Andreas M., Liniger, Mark A., Croci-Maspoli, Mischa, Scherrer, Simon C., Appenzeller, Christof
• Format: Article
• Language: English
• Subjects: 21st century; Alps; Atmospheric Sciences; Climate change; Climate Change/Climate Change Impacts; Climate models; Climatology. Bioclimatology. Climate change; Computer simulation; Datasets; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; Emission; Emissions; Environmental impact; Exact sciences and technology; External geophysics; General circulation models; Global warming; Kriging; Meteorology; Precipitation; Regional; Regions; Simulation; Temperature; Topography; Trends
• ISSN: 0165-0009; 1573-1480
• DOI: 10.1007/s10584-014-1144-x

There is a growing need of the climate change impact modeling and adaptation community to have more localized climate change scenario information available over complex topography such as in Switzerland. A gridded dataset of expected future climate change signals for seasonal averages of daily mean temperature and precipitation in Switzerland is presented. The basic scenarios are taken from the CH2011 initiative. In CH2011, a Bayesian framework was applied to obtain probabilistic scenarios for three regions within Switzerland. Here, the results for two additional Alpine sub-regions are presented. The regional estimates have then been downscaled onto a regular latitude-longitude grid with a resolution of 0.02° or roughly 2 km. The downscaling procedure is based on the spatial structure of the climate change signals as simulated by the underlying regional climate models and relies on a Kriging with external drift using height as auxiliary predictor. The considered emission scenarios are A1B, A2 and the mitigation scenario RCP3PD. The new dataset shows an expected warming of about 1 to 6 °C until the end of the 21st century, strongly depending on the scenario and the lead time. Owing to a large vertical gradient, the warming is about 1 °C stronger in the Alps than in the Swiss lowlands. In case of precipitation, the projection uncertainty is large and in most seasons precipitation can increase or decrease. In summer a distinct decrease of precipitation can be found, again strongly depending on the emission scenario.