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BCM2.0, (2005): atmosphere: ARPEGE V3 T63L31 (cy 22b+); ocean: NERSC-MICOM V1.0 (based on MICOM V2.8), 35 vertical layers, 1.5(E-W) X 0.5(N-S) deg. res. near equator with gradual transformation to square grid cells away from equator; sea ice: NERSC Sea Ice Model (Viscous-plastic + thermodynamic), 4 gridcells per ocean grid cell; land: ISBA ARPEGE V3 version. Experiment was initiated from model year 85 (nominal year 1850) of the control simulation (with bcm_experiment_name: PC3). The time varying forcing agents were varied based upon observations and reconstructions for the late 19th and 20th centuries. Varying forcing agents: CO2,CH4,N2O, CFC11(including other CFCs and HFCs),CFC12 and sulfate aerosols (Boucher data, only direct effect). Non-varying forcing agents: Background aerosols: black carbon, sea salt, desert dust, stratospheric and tropospheric ozone, solar irradiance (1368 W/m2) and the distribution of land cover types. No volcanic aerosols. 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sulfate aerosol https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ http://w3id.org/ro/earth-science#Sentence BCM2.0, (2005) atmosphere: ARPEGE V3 T63L31 (cy 22b+ ocean: NERSC-MICOM V1.0 (based on MICOM V2.8) 35 vertical layers, 1.5(E-W) X 0.5(N-S) deg. res. near equator with gradual transformation to square grid cells away from equator; sea ice: NERSC Sea Ice Model (Viscous-plastic + thermodynamic) 4 gridcells per ocean grid cell; land: ISBA ARPEGE V3 version. https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ http://w3id.org/ro/earth-science#Sentence Experiment was initiated from model year 85 (nominal year 1850) of the control simulation (with bcm_experiment_name: PC3) The time varying forcing agents were varied based upon observations and reconstructions for the late 19th and 20th centuries. https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ http://w3id.org/ro/earth-science#Sentence Ocean and atmosphere output of the Bergen Climate Model experiment PC3. https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ http://w3id.org/ro/earth-science#TimeReference 1368 https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ http://w3id.org/ro/earth-science#TimeReference 2005 https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ http://w3id.org/ro/earth-science#TimeReference year 1850 https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/ro#ResearchObject https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/roevo#LiveRO https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/Dataset https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://w3id.org/ro/earth-science#DataResearchObject https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#DataResearchObject https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ https://w3id.org/contentdesc#Domain chemistry https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ https://w3id.org/contentdesc#Domain organic chemistry https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ https://w3id.org/contentdesc#Domain physics https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/ https://www.w3.org/ns/iana/link-relations/relation#cite-as Tore Furevik, Mats Bentsen, Helge Drange, Ina Karin Thorstensen Kindem, Nils Gunnar Kvamstø, Asgeir Sorteberg, Frode Flatøy, Ingo Bethke, Odd Helge Otterå, and Geophysical Institute, University of Bergen (GFI/UiB). "Ocean and atmosphere output of the Bergen Climate Model experiment PC3." ROHub. 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K., Kvamstø, N. G., Sorteberg, A., Flatøy, F., Bethke, I., Otterå, O. H., Geophysical Institute, University of Bergen, NORCE Norwegian Research Centre, Nansen Environmental and Remote Sensing Centre, Bjerknes Centre for Climate Research (2020).Ocean and atmosphere output of the Bergen Climate Model experiment PC3 [Data set]. Norstore. https://doi.org/10.11582/2020.00046 https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/resources/6d0a2024-12f1-47b4-9409-9de0ec6c260c http://purl.org/dc/terms/rightsHolder Mats Bentsen https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/resources/6d0a2024-12f1-47b4-9409-9de0ec6c260c http://purl.org/dc/terms/type Simulation https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/resources/6d0a2024-12f1-47b4-9409-9de0ec6c260c http://schema.org/author mailto:georgehadib@gmail.com https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/resources/6d0a2024-12f1-47b4-9409-9de0ec6c260c http://schema.org/contentUrl https://archive.sigma2.no/pages/public/datasetDetail.jsf?id=10.11582/2020.00046 https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/resources/6d0a2024-12f1-47b4-9409-9de0ec6c260c http://schema.org/creator mailto:georgehadib@gmail.com https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/resources/6d0a2024-12f1-47b4-9409-9de0ec6c260c http://schema.org/dateCreated 2020-09-22 00:00:00 https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/resources/6d0a2024-12f1-47b4-9409-9de0ec6c260c http://schema.org/dateModified 2022-03-22 02:41:14.581401+00:00 https://w3id.org/ro-id/c52a1daa-7c5b-41d1-9f68-d372e12529f0/resources/6d0a2024-12f1-47b4-9409-9de0ec6c260c http://schema.org/description Pre-industrial control experiment prepared for the IPCC Fourth Assessment Report. BCM2.0, (2005): atmosphere: ARPEGE V3 T63L31 (cy 22b+); ocean: NERSC-MICOM V1.0 (based on MICOM V2.8), 35 vertical layers, 1.5(E-W) X 0.5(N-S) deg. res. near equator with gradual transformation to square grid cells away from equator; sea ice: NERSC Sea Ice Model (Viscous-plastic + thermodynamic), 4 gridcells per ocean grid cell; land: ISBA ARPEGE V3 version. Experiment was initiated from model year 85 (nominal year 1850) of the control simulation (with bcm_experiment_name: PC3). The time varying forcing agents were varied based upon observations and reconstructions for the late 19th and 20th centuries. Varying forcing agents: CO2,CH4,N2O, CFC11(including other CFCs and HFCs),CFC12 and sulfate aerosols (Boucher data, only direct effect). Non-varying forcing agents: Background aerosols: black carbon, sea salt, desert dust, stratospheric and tropospheric ozone, solar irradiance (1368 W/m2) and the distribution of land cover types. No volcanic aerosols. 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