[2]
;
Castrodíez, Yolanda
[2]
;
Esteban-Parra, María Jesús
[2]
;
Gámiz-Fortis, Sonia Raquel
[2]
Granada, España
In order to obtain information about the evolution of climate variables at regional scale, the downscaling method is carried out by using Regional Climate Models (RCMs). It increases the data spatial resolution from the Global Climate Models (GCMs) output data, which present low spatial resolutions, managing to generate climate simulations with spatial resolutions below to 10 km. For it, the GCM outputs are used as boundary conditions in the regional model. Furthermore, PseudoGlobal Warming method (PGW) appears as a simulation strategy in the regional climate modeling, with the aim of decreasing computational costs, improving the flexibility of simulations and avoiding certain GCM bias, especially at regional scales. Basically, this method consists in coupling differences between future and present climate given by GCMs with boundary conditions given by reanalysis data. In this sense, in order to use the PWG method in the climate change downscaled projections over the Iberian Peninsula, it is important to evaluate the skill of GCMs for the representation of the most important climate aspects in the study area. In this work this evaluation is carried out from the available CMIP6 GCMs by applying different statistical technics. In the first part, the ability of the different GCMs for simulating the North Atlantic Oscillation pattern is considered by applying a Principal Component Analysis (PCA) to sea level pressure (SLP) winter data for the period 1960-2014. In the second part, differences in the SLP averaged field over the North Atlantic region between the 24 CMIP6 GCM outputs and the observations were analyzed. The results of these analyses showed a good agreement of every GCM for the SLP, therefore all them could be part of an ensemble for the subsequent PGW application.
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