Harmonized evaluation of daily precipitation downscaled using SDSM and WRF+WRFDA models over the Iberian Peninsula
dc.contributor.author | González Rojí, Santos José | |
dc.contributor.author | Wilby, Robert L. | |
dc.contributor.author | Sáenz Aguirre, Jon | |
dc.contributor.author | Ibarra Berastegi, Gabriel | |
dc.date.accessioned | 2020-01-29T09:35:02Z | |
dc.date.available | 2020-01-29T09:35:02Z | |
dc.date.issued | 2019-08 | |
dc.identifier.citation | Climate Dynamics 53(3-4) : 1413-1433 (2019) | es_ES |
dc.identifier.issn | 0930-7575 | |
dc.identifier.issn | 1432-0894 | |
dc.identifier.uri | http://hdl.handle.net/10810/39227 | |
dc.description.abstract | There have been numerous statistical and dynamical downscaling model comparisons. However, differences in model skill can be distorted by inconsistencies in experimental set-up, inputs and output format. This paper harmonizes such factors when evaluating daily precipitation downscaled over the Iberian Peninsula by the Statistical DownScaling Model (SDSM) and two configurations of the dynamical Weather Research and Forecasting Model (WRF) (one with data assimilation (D) and one without (N)). The ERA-Interim reanalysis at 0.75 degrees resolution provides common inputs for spinning-up and driving the WRF model and calibrating SDSM. WRF runs and SDSM output were evaluated against ECA&D stations, TRMM, GPCP and EOBS gridded precipitation for 2010-2014 using the same suite of diagnostics. Differences between WRF and SDSM are comparable to observational uncertainty, but the relative skill of the downscaling techniques varies with diagnostic. The SDSM ensemble mean, WRF-D and ERAI have similar correlation scores (r=0.45-0.7), but there were large variations amongst SDSM ensemble members (r=0.3-0.6). The best Linear Error in Probability Space (LEPS=0.001-0.007) and simulations of precipitation amount were achieved by individual members of the SDSM ensemble. However, the Brier Skill Score shows these members do not improve the prediction by ERA-Interim, whereas precipitation occurrence is reproduced best by WRF-D. Similar skill was achieved by SDSM when applied to station or gridded precipitation data. Given the greater computational demands of WRF compared with SDSM, clear statements of expected value-added are needed when applying the former to climate impacts and adaptation research. | es_ES |
dc.description.sponsorship | This work was supported by Grants (CGL2013-45198-C2-1-R and CGL2016-76561-R, MINECO/ERDF, UE). S.J.G.R. was supported by a FPI Postdoctoral Research Grant (MINECO, BES-2014-069977). Additional funding was received from the University of the Basque Country (UPV/EHU, GIU 17/002). Intensive computational resources used in the project were provided by I2BASQUE. The authors thank the creators of the WRF/ARW and WRFDA systems for making them freely available to the community. The authors acknowledge the E-OBS dataset from the EU-FP6 project ENSEMBLES and the data providers in the ECA&D project. NOAA_OI_SST_V2 data provided by the NOAA/OAR/ESRL PSD, Boulder, Colorado, USA. Comments by two anonymous reviewers have significantly improved the manuscript. | es_ES |
dc.language.iso | eng | es_ES |
dc.publisher | Springer | es_ES |
dc.relation | info:eu-repo/grantAgreement/MINECO/CGL2013-45198-C2-1-R | es_ES |
dc.relation | info:eu-repo/grantAgreement/MINECO/CGL2016-76561-R | es_ES |
dc.rights | info:eu-repo/semantics/openAccess | es_ES |
dc.rights.uri | http://creativecommons.org/licenses/by/3.0/es/ | * |
dc.subject | regional climate modelling | es_ES |
dc.subject | dynamical downscaling | es_ES |
dc.subject | statistical downscaling | es_ES |
dc.subject | precipitation | es_ES |
dc.subject | WRF | es_ES |
dc.subject | SDSM | es_ES |
dc.subject | iberian peninsula | es_ES |
dc.subject | data assimilation | es_ES |
dc.subject | 3dvar data assimilation | es_ES |
dc.subject | bias correction | es_ES |
dc.subject | interannual variability | es_ES |
dc.subject | extreme precipitation | es_ES |
dc.subject | atmospheric moisture | es_ES |
dc.subject | change scenarios | es_ES |
dc.subject | winter rainfall | es_ES |
dc.subject | water-resources | es_ES |
dc.subject | southern europe | es_ES |
dc.title | Harmonized evaluation of daily precipitation downscaled using SDSM and WRF+WRFDA models over the Iberian Peninsula | es_ES |
dc.type | info:eu-repo/semantics/article | es_ES |
dc.rights.holder | This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. | es_ES |
dc.rights.holder | Atribución 3.0 España | * |
dc.relation.publisherversion | https://link.springer.com/article/10.1007%2Fs00382-019-04673-9 | es_ES |
dc.identifier.doi | 10.1007/s00382-019-04673-9 | |
dc.departamentoes | Física aplicada II | es_ES |
dc.departamentoes | Ingeniería nuclear y mecánica de fluidos | es_ES |
dc.departamentoeu | Fisika aplikatua II | es_ES |
dc.departamentoeu | Ingeniaritza nuklearra eta jariakinen mekanika | es_ES |
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