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The resolution of a RCM is not enough for most hydrologicalmodels, thus they need to be further downscaled and bias-corrected(Christensen et al., 2008) to produce atmospheric forcingsat the adequate resolution (10 km) (Wood et al., 2004). Thus it isnecessary to further downscale the output of these models andto develop methods to reconstruct the regional climate in relationto climate on a larger scale.
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