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Hydrological change--climate change impact simulations for Sweden
Johan Andréasson1, Sten Bergström, Bengt Carlsson
1Department of Research and Development, Swedish Meteorological and Hydrological Institute, Norrköping. johan.andreasson@smhi.se
Ambio
|July 22, 2004
Summary
Climate change will alter hydrological systems, with impacts varying by region. This study shows Swedish river flow changes significantly differ between northern and southern basins, depending on climate models and emissions scenarios.
Area of Science:
- Environmental science
- Hydrology
- Climate science
Background:
- The enhanced greenhouse effect is projected to alter global hydrological systems.
- Hydrological changes will exhibit significant regional variations, necessitating local and regional impact assessments.
- Understanding these impacts is crucial for effective climate change adaptation strategies.
Purpose of the Study:
- To assess the hydrological impacts of climate change across various Swedish river basins.
- To compare different methods for translating climate model outputs to hydrological models.
- To analyze the influence of climate model choice and emissions scenarios on projected hydrological changes.
Main Methods:
- Utilized regional climate model (RCM) scenarios from the Swedish Regional Climate Modelling Programme (SWECLIM).
- Employed multiple methods for downscaling climate change signals from global climate models (GCMs) to RCMs.
- Conducted hydrological model simulations using the downscaled climate data for Swedish basins.
Main Results:
- Projected hydrological changes in Swedish basins show considerable subregional variations, particularly between northern and southern Sweden.
- The choice of GCM significantly influences RCM boundary conditions and, consequently, projected hydrological impacts.
- The selection of anthropogenic emissions scenarios also plays a critical role in determining the magnitude of hydrological change.
Conclusions:
- Subregional hydrological impacts of climate change in Sweden are highly variable.
- Projected river flow alterations are sensitive to both the GCM used for boundary conditions and the chosen emissions scenario.
- Future hydrological assessments must account for uncertainties associated with climate model selection and emissions pathways.