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Added value of EURO-CORDEX high-resolution downscaling over the Iberian Peninsula revisited – Part 1: Precipitation
Over the years, higher-resolution regional climate model simulations have emerged owing to the large increase in computational resources. The 12 km resolution from the Coordinated Regional Climate Downscaling Experiment for the European domain (EURO-CORDEX) is a reference, which includes a larger mu...
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Published in: | Geoscientific Model Development 2022-04, Vol.15 (6), p.2635-2652 |
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Main Authors: | , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Over the years, higher-resolution regional climate model
simulations have emerged owing to the large increase in computational
resources. The 12 km resolution from the Coordinated Regional Climate
Downscaling Experiment for the European domain (EURO-CORDEX) is a reference,
which includes a larger multi-model ensemble at a continental scale while
spanning at least a 130-year period. These simulations are computationally
demanding but do not always reveal added value. In this study, a recently
developed regular gridded dataset and a new metric for added value
quantification, the distribution added value (DAV), are used to assess the
precipitation of all available EURO-CORDEX hindcast (1989–2008) and
historical (1971–2005) simulations. This approach enables a direct
comparison between the higher-resolution regional model runs against their
forcing global model or ERA-Interim reanalysis with respect to their
probability density functions. This assessment is performed for the Iberian
Peninsula. Overall, important gains are found for most cases, particularly
in precipitation extremes. Most hindcast models reveal gains above 15 %,
namely for wintertime, while for precipitation extremes values above 20 %
are reached for the summer and autumn. As for the historical models,
although most pairs display gains, regional models forced by two general circulation models (GCMs) reveal
losses, sometimes around −5 % or lower, for the entire year. However, the
spatialization of the DAV is clear in terms of added value for
precipitation, particularly for precipitation extremes with gains well above
100 %. |
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ISSN: | 1991-9603 1991-959X 1991-962X 1991-9603 1991-962X |
DOI: | 10.5194/gmd-15-2635-2022 |