{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360294674048782848.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5194/gmd-2019-350"}}],"resourceType":"preprint","dc:title":[{"@value":"HighResMIP versions of EC-Earth: EC-Earth3P and EC-Earth3P-HR. Description, model performance, data handling and validation"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Abstract. A new global high-resolution coupled climate model, EC-Earth3P-HR has been developed by the EC-Earth consortium, with a resolution of approximately 40 km for the atmosphere and 0.25 degree for the ocean, alongside with a standard resolution version of the model, EC-Earth3P (80 km atmosphere, 1.0 degree ocean). The model forcing and simulations follow the HighResMIP protocol. According to this protocol all simulations are made with both high and standard resolutions. The model has been optimized with respect to scalability, performance, data-storage and post-processing. In accordance with the HighResMIP protocol no specific tuning for the high resolution version has been applied. Increasing horizontal resolution does not result in a general reduction of biases and overall improvement of the variability, and deteriorating impacts can be detected for specific regions and phenomena such as some Euro-Atlantic weather regimes, whereas others such as El Niño-Southern Oscillation show a clear improvement in their spatial structure. The omission of specific tuning might be responsible for this. The shortness of the spin-up, as prescribed by the HighResMIP protocol, prevented the model to reach equilibrium. The trend in the control and historical simulations, however, appeared to be similar, resulting in a warming trend, obtained by subtracting the control from the historical simulation, close to the observational one.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380294674048782992","@type":"Researcher","foaf:name":[{"@value":"Rein Haarsma"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782990","@type":"Researcher","foaf:name":[{"@value":"Mario Acosta"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782851","@type":"Researcher","foaf:name":[{"@value":"Rena Bakhshi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782849","@type":"Researcher","foaf:name":[{"@value":"Pierre-Antoine Bretonnière Bretonnière"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782987","@type":"Researcher","foaf:name":[{"@value":"Louis-Philippe Caron"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782976","@type":"Researcher","foaf:name":[{"@value":"Miguel Castrillo"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782855","@type":"Researcher","foaf:name":[{"@value":"Susanna Corti"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782993","@type":"Researcher","foaf:name":[{"@value":"Paolo Davini"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782983","@type":"Researcher","foaf:name":[{"@value":"Eleftheria Exarchou"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782991","@type":"Researcher","foaf:name":[{"@value":"Federico Fabiano"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782980","@type":"Researcher","foaf:name":[{"@value":"Uwe Fladrich"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782988","@type":"Researcher","foaf:name":[{"@value":"Ramon Fuentes Franco"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782848","@type":"Researcher","foaf:name":[{"@value":"Javier García-Serrano"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782978","@type":"Researcher","foaf:name":[{"@value":"Jost von Hardenberg"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782985","@type":"Researcher","foaf:name":[{"@value":"Torben Koenigk"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782852","@type":"Researcher","foaf:name":[{"@value":"Xavier Levine"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782981","@type":"Researcher","foaf:name":[{"@value":"Virna Meccia"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782986","@type":"Researcher","foaf:name":[{"@value":"Twan van Noije"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782850","@type":"Researcher","foaf:name":[{"@value":"Gijs van den Oord"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782979","@type":"Researcher","foaf:name":[{"@value":"Froila M. Palmeiro"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782977","@type":"Researcher","foaf:name":[{"@value":"Mario Rodrigo"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782982","@type":"Researcher","foaf:name":[{"@value":"Yohan Ruprich-Robert"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782854","@type":"Researcher","foaf:name":[{"@value":"Philippe Le Sager"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782984","@type":"Researcher","foaf:name":[{"@value":"Étienne Tourigny"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782856","@type":"Researcher","foaf:name":[{"@value":"Shiyu Wang"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782853","@type":"Researcher","foaf:name":[{"@value":"Michiel van Weele"}]},{"@id":"https://cir.nii.ac.jp/crid/1380294674048782989","@type":"Researcher","foaf:name":[{"@value":"Klaus Wyser"}]}],"publication":{"dc:publisher":[{"@value":"Copernicus GmbH"}],"prism:publicationDate":"2020-03-02"},"reviewed":"false","dc:rights":["https://creativecommons.org/licenses/by/4.0/"],"createdAt":"2020-03-02","modifiedAt":"2025-01-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360853567779080064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Projected Future Changes in Tropical Cyclones Using the CMIP6 HighResMIP Multimodel Ensemble"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892101960576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evaluation of the contribution of tropical cyclone seeds to changes in tropical cyclone frequency due to global warming in high-resolution multi-model ensemble simulations"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.5194/gmd-2019-350"},{"@type":"CROSSREF","@value":"10.1029/2020gl088662_references_DOI_ERqpImGUDGnzFeQY6s5YGCNRkmw"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00397-1_references_DOI_ERqpImGUDGnzFeQY6s5YGCNRkmw"}]}