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http://schema.org/dateCreated 2022-03-22 02:29:57.775650+00:00 https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/ http://schema.org/dateModified 2025-03-05 12:49:09.459424+00:00 https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/ http://schema.org/datePublished 2022-03-22 02:29:57.775650+00:00 https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/ http://schema.org/description Output of the sea ice, marine biogeochemistry and physical fields of the last 30 years (year 5571-5600) of a Last Glacial Maximum (LGM) simulation. This simulation was performed with NorESM-OC and includes a sea ice model, ocean circulation model as well as full biogeochemistry with the carbon isotopes (Tjiputra et al., 2020, Geoscientific Model Development). In order to obtain the LGM state, several adjustments were made to the model forcing: 1) use of a glacial atmospheric dust field (Lambert et al., 2015), 2) tuning of the surface salinity restoring (procedure described in Climate of the Past - Morée et al., 2020 and its supplement) 3) adjustment of the land-ocean mask by reducing the ocean volume with ~116m (procedure described in Climate of the Past - Morée et al., 2020 and its supplement), and 4) adjustment of the atmospheric Normal Year Forcing fields to an LGM approximation by applying the atmospheric LGM-PI anomalies of Morée and Schwinger (2020, Earth System Science Data, version 1) to the models original ('pre-industrial') atmospheric forcing. 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"Ocean output of NorESM-OC simulation of the Last Glacial Maximum (21 kya)." ROHub. 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http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/dc/terms/BibliographicResource https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/resources/b52828d8-a4a0-48d5-9836-ddd33e2bbad3 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/wf4ever#Resource https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/resources/b52828d8-a4a0-48d5-9836-ddd33e2bbad3 http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/MediaObject https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/resources/c455f59a-a309-48ed-822b-38829b25e210 http://purl.org/dc/terms/bibliographicCitation Morée, A., Schwinger, J., Bethke, I., Heinze, C., Geophysical Institute, University of Bergen, NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research (2020).Ocean output of NorESM-OC simulation of the Last Glacial Maximum (21 kya) [Data set]. Norstore. https://doi.org/10.11582/2020.00062 https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/resources/c455f59a-a309-48ed-822b-38829b25e210 http://purl.org/dc/terms/rightsHolder Anne Morée https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/resources/c455f59a-a309-48ed-822b-38829b25e210 http://purl.org/dc/terms/type Simulation https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/resources/c455f59a-a309-48ed-822b-38829b25e210 http://schema.org/author mailto:georgehadib@gmail.com https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/resources/c455f59a-a309-48ed-822b-38829b25e210 http://schema.org/contentUrl https://archive.sigma2.no/pages/public/datasetDetail.jsf?id=10.11582/2020.00062 https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/resources/c455f59a-a309-48ed-822b-38829b25e210 http://schema.org/creator mailto:georgehadib@gmail.com https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/resources/c455f59a-a309-48ed-822b-38829b25e210 http://schema.org/dateCreated 2020-12-07 00:00:00 https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/resources/c455f59a-a309-48ed-822b-38829b25e210 http://schema.org/dateModified 2022-03-22 02:30:57.006487+00:00 https://w3id.org/ro-id/fbeaadb1-8c0d-4ef9-8141-3337d99a9fad/resources/c455f59a-a309-48ed-822b-38829b25e210 http://schema.org/description Output of the sea ice, marine biogeochemistry and physical fields of the last 30 years (year 5571-5600) of a Last Glacial Maximum (LGM) simulation. This simulation was performed with NorESM-OC and includes a sea ice model, ocean circulation model as well as full biogeochemistry with the carbon isotopes (Tjiputra et al., 2020, Geoscientific Model Development). In order to obtain the LGM state, several adjustments were made to the model forcing: 1) use of a glacial atmospheric dust field (Lambert et al., 2015), 2) tuning of the surface salinity restoring (procedure described in Climate of the Past - Morée et al., 2020 and its supplement) 3) adjustment of the land-ocean mask by reducing the ocean volume with ~116m (procedure described in Climate of the Past - Morée et al., 2020 and its supplement), and 4) adjustment of the atmospheric Normal Year Forcing fields to an LGM approximation by applying the atmospheric LGM-PI anomalies of Morée and Schwinger (2020, Earth System Science Data, version 1) to the models original ('pre-industrial') atmospheric forcing. 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