Evaluating the performance of CMIP3 and CMIP5 global climate models over the north-east Atlantic region
Performance of CMIP3 and CMIP5 global climate models over the north-east Atlantic region
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Pérez García, Jorge; Menéndez García, Melisa


Fecha
2014-02Derechos
© 2014, Springer-Verlag Berlin Heidelberg. This version of the article has been accepted for publication, after peer review and is subject to Springer Nature's AM terms of use, but is not the Version of Record and does not reflect post-acceptance improvements, or any corrections. The Version of Record is available online at: http://dx.doi.org/10.1007/s00382-014-2078-8
Publicado en
Climate Dynamics, 2014, 43(9-10), 2663-2680
Editorial
Springer
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Palabras clave
Downscaling
General circulation models
Projections
Skill
Weather types
Resumen/Abstract
One of the main sources of uncertainty in estimating climate projections affected by global warming
is the choice of the global climate model (GCM). The aim of this study is to evaluate the skill of GCMs from CMIP3 and CMIP5 databases in the north-east Atlantic Ocean region. It is well known that the seasonal and interannual variability of surface inland variables (e.g. precipitation and snow) and ocean variables (e.g. wave height and storm surge) are linked to the atmospheric circulation patterns. Thus, an automatic synoptic classification, based on weather types, has been used to assess whether GCMs are able to reproduce spatial patterns and climate variability. Three important factors have been analyzed: the skill of GCMs to reproduce the synoptic situations, the skill of GCMs to reproduce the historical inter-annual variability and the consistency of GCMs experiments during twentyfirst century projections. The results of this analysis indicate that the most skilled GCMs in the study region are UKMO-HadGEM2, ECHAM5/MPI-OM and MIROC3.2(hires) for CMIP3 scenarios and ACCESS1.0, ECEARTH, HadGEM2-CC, HadGEM2-ES and CMCC-CM for CMIP5 scenarios. These models are therefore recommended for the estimation of future regional multi-model projections of surface variables driven by the atmospheric circulation in the north-east Atlantic Ocean region.
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