Robust changes and sources of uncertainty in the projected hydrological regimes of Swiss catchments

被引:182
作者
Addor, Nans [1 ]
Roessler, Ole [2 ,3 ]
Koeplin, Nina [2 ,3 ]
Huss, Matthias [4 ]
Weingartner, Rolf [2 ,3 ]
Seibert, Jan [1 ,5 ]
机构
[1] Univ Zurich, Dept Geog, Zurich, Switzerland
[2] Univ Bern, Oeschger Ctr Climate Change Res, Bern, Switzerland
[3] Univ Bern, Dept Geog, Bern, Switzerland
[4] Univ Fribourg, Dept Geosci, CH-1700 Fribourg, Switzerland
[5] Uppsala Univ, Dept Earth Sci, Uppsala, Sweden
基金
瑞士国家科学基金会;
关键词
climate change; catchment discharge; uncertainty assessment; robust projections; European Alps; impacts mitigation; MODEL INTERCOMPARISON PROJECT; CLIMATE-CHANGE SIGNALS; RUNOFF-MODEL; WATERSHED MODEL; CHANGE IMPACTS; STREAMFLOW; ENSEMBLE; SNOW; PRECIPITATION; SIMULATION;
D O I
10.1002/2014WR015549
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Projections of discharge are key for future water resources management. These projections are subject to uncertainties, which are difficult to handle in the decision process on adaptation strategies. Uncertainties arise from different sources such as the emission scenarios, the climate models and their postprocessing, the hydrological models, and the natural variability. Here we present a detailed and quantitative uncertainty assessment, based on recent climate scenarios for Switzerland (CH2011 data set) and covering catchments representative for midlatitude alpine areas. This study relies on a particularly wide range of discharge projections resulting from the factorial combination of 3 emission scenarios, 10-20 regional climate models, 2 postprocessing methods, and 3 hydrological models of different complexity. This enabled us to decompose the uncertainty in the ensemble of projections using analyses of variance (ANOVA). We applied the same modeling setup to six catchments to assess the influence of catchment characteristics on the projected streamflow, and focused on changes in the annual discharge cycle. The uncertainties captured by our setup originate mainly from the climate models and natural climate variability, but the choice of emission scenario plays a large role by the end of the 21st century. The contribution of the hydrological models to the projection uncertainty varied strongly with catchment elevation. The discharge changes were compared to the estimated natural decadal variability, which revealed that a climate change signal emerges even under the lowest emission scenario (RCP2.6) by the end of the century. Limiting emissions to RCP2.6 levels would nevertheless reduce the largest regime changes by the end of the century by approximately a factor of two, in comparison to impacts projected for the high emission scenario SRES A2. We finally show that robust regime changes emerge despite the projection uncertainty. These changes are significant and are consistent across a wide range of scenarios and catchments. We propose their identification as a way to aid decision making under uncertainty.
引用
收藏
页码:7541 / 7562
页数:22
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