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Volume 19, issue 7
Hydrol. Earth Syst. Sci., 19, 3217–3238, 2015
https://doi.org/10.5194/hess-19-3217-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 19, 3217–3238, 2015
https://doi.org/10.5194/hess-19-3217-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 24 Jul 2015

Research article | 24 Jul 2015

Impacts of climate change on temperature, precipitation and hydrology in Finland – studies using bias corrected Regional Climate Model data

T. Olsson et al.
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Cited articles  
Andréasson, J., Bergström, S., Carlsson, B., Graham, L., and Lindström, G.: Hydrological change – climate change impact simulations for Sweden, Ambio, 33, 228–234, 2004.
Beldring, S., Engen-Skaugen, T., Førland, E., and Roald, L.: Climate change impacts on hydrological processes in Norway based on two methods for transferring RCM results to meteorological station sites, Tellus A, 60, 439–450, 2008.
Bergström, S.: Development and application of a conceptual runoff model for Scandinavian catchments, SMHI, Norrköping, Report RHO No. 7, 134 pp., 1976.
Castro, M., Gallardo, C., Jylhä, K., and Tuomenvirta, H.: The use of a climate-type classification for assessing climate change effects in Europe from an Ensemble of nine regional climate models, Climatic Change, 81, 329–341, https://doi.org/10.1007/s10584-006-9224-1, 2007.
Christensen, J. H., Boberg, F., Christensen, O. B., and Lucas-Picher, P.: On the need for bias correction of regional climate change projections of temperature and precipitation, Geophys. Res. Lett., 35, L20709, https://doi.org/10.1029/2008GL035694, 2008.
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With most scenarios the DBS method used preserves the temperature and precipitation trends of the uncorrected RCM data and produces more realistic projections for mean annual and seasonal changes in discharges than the uncorrected RCM data in Finland. However, if the biases in the mean or the standard deviation of the uncorrected temperatures are large, significant biases after DBS adjustment may remain or temperature trends may change, increasing the uncertainty of climate change projections.
With most scenarios the DBS method used preserves the temperature and precipitation trends of...
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