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dc.contributor.authorBaño Medina, Jorge 
dc.contributor.authorIturbide Martínez de Albéniz, Maialen 
dc.contributor.authorFernández Fernández, Jesús (matemático) 
dc.contributor.authorGutiérrez Llorente, José Manuel
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2025-10-10T08:28:05Z
dc.date.available2025-10-10T08:28:05Z
dc.date.issued2024-10
dc.identifier.issn2769-7525
dc.identifier.otherPID2019-111481RB-I00es_ES
dc.identifier.otherPID2020- 116595RB-I00es_ES
dc.identifier.urihttps://hdl.handle.net/10902/37725
dc.description.abstractRegional climate models (RCMs) are essential tools for simulating and studying regional climate variability and change. However, their high computational cost limits the production of comprehensive ensembles of regional climate projections covering multiple scenarios and driving Global climate models (GCMs) across regions. RCM emulators based on deep learning models have recently been introduced as a cost-effective and promising alternative that requires only short RCM simulations to train the models. Therefore, evaluating their transferability to different periods, scenarios, and GCMs becomes a pivotal and complex task in which the inherent biases of both GCMs and RCMs play a significant role. Here, we focus on this problem by considering the two different emulation approaches introduced in the literature as perfect and imperfect, that we here refer to as perfect prognosis (PP) and model output statistics (MOS), respectively, following the well-established downscaling terminology. In addition to standard evaluation techniques, we expand the analysis with methods from the field of explainable artificial intelligence (XAI), to assess the physical consistency of the empirical links learnt by the models.We find that both approaches are able to emulate certain climatological properties of RCMs for different periods and scenarios (soft transferability), but the consistency of the emulation functions differs between approaches. Whereas PP learns robust and physically meaningful patterns, MOS results are GCM dependent and lack physical consistency in some cases. Both approaches face problems when transferring the emulation function to other GCMs (hard transferability), due to the existence of GCM-dependent biases. This limits their applicability to build RCM ensembles. We conclude by giving prospects for future applications.es_ES
dc.description.sponsorshipThis work is part of IMPETUS4-CHANGE, funded by the European Union’s Horizon Europe research and innovation programme under Grant Agreement 101081555. J. M. G. and J. F. acknowledge support from MCIN/AEI/10.13039/501100011033, which funded projects ATLAS (PID2019-111481RB-I00) and CORDyS (PID2020-116595RB-I00), respectively. We would like to express our gratitude to the anonymous reviewers for their valuable feedback and insightful comments, which greatly contributed to the improvement of this manuscript. We extend our special thanks to Antoine Doury for his valuable suggestions and ideas, which clarified the methodology and were also incorporated into the conclusions of this work as potential lines of further research.es_ES
dc.format.extent15 p.es_ES
dc.language.isoenges_ES
dc.publisherAmerican Meteorological Societyes_ES
dc.rights© 2024 American Meteorological Society. This published article is licensed under the terms of the default AMS reuse license. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).es_ES
dc.sourceArtificial Intelligence for the Earth Systems, 2024, 3(4), e230099es_ES
dc.subject.otherDownscalinges_ES
dc.subject.otherNeural networkses_ES
dc.subject.otherClimate variabilityes_ES
dc.titleTransferability and explainability of deep learning emulators for regional climate model projections: perspectives for future applicationses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherVersionhttps://doi.org/10.1175/AIES-D-23-0099.1es_ES
dc.rights.accessRightsopenAccesses_ES
dc.identifier.DOI10.1175/AIES-D-23-0099.1
dc.type.versionpublishedVersiones_ES


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