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Evaluation of uncertainties in the CRCM-simulated North American climate
Authors:Ramón de Elía  Daniel Caya  Hélène Côté  Anne Frigon  Sébastien Biner  Michel Giguère  Dominique Paquin  Richard Harvey  David Plummer
Affiliation:(1) Climate Simulations Team, Consortium Ouranos, 550 Sherbrooke street West, 19th floor, West tower, Montreal, QC, Canada, H3A 1B9;(2) Canadian Centre for Climate Modelling and Analysis, Meteorological Service of Canada, Victoria, BC, Canada
Abstract:This work is a first step in the analysis of uncertainty sources in the RCM-simulated climate over North America. Three main sets of sensitivity studies were carried out: the first estimates the magnitude of internal variability, which is needed to evaluate the significance of changes in the simulated climate induced by any model modification. The second is devoted to the role of CRCM configuration as a source of uncertainty, in particular the sensitivity to nesting technique, domain size, and driving reanalysis. The third study aims to assess the relative importance of the previously estimated sensitivities by performing two additional sensitivity experiments: one, in which the reanalysis driving data is replaced by data generated by the second generation Coupled Global Climate Model (CGCM2), and another, in which a different CRCM version is used. Results show that the internal variability, triggered by differences in initial conditions, is much smaller than the sensitivity to any other source. Results also show that levels of uncertainty originating from liberty of choices in the definition of configuration parameters are comparable among themselves and are smaller than those due to the choice of CGCM or CRCM version used. These results suggest that uncertainty originated by the CRCM configuration latitude (freedom of choice among domain sizes, nesting techniques and reanalysis dataset), although important, does not seem to be a major obstacle to climate downscaling. Finally, with the aim of evaluating the combined effect of the different uncertainties, the ensemble spread is estimated for a subset of the analysed simulations. Results show that downscaled surface temperature is in general more uncertain in the northern regions, while precipitation is more uncertain in the central and eastern US.
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