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We obtain a steady state ocean circulation by running the time-dependent, nonlinear model to equi- librium using restoring boundary conditions on surface temperature. This is simulated by MITgcm using a 2◦ × 2◦ spherical polar grid. We examine how this circulation relates to theories of the surface - and the abyssal circulation. These theories include the linear thermocline theory and Stommel and Arons theory. An important factor in returning the deep water to the surface, is the diapycnal mixing. Why this is important will be discussed. The reasons why and where the deep water upwells, are well debated. We find that positive vertical velocity mainly occurs at the western boundaries, where both the currents in the abyss and at the surface are strong. The simulated ocean circulation contains many of the observed currents in the world, like the Antarctic Circumpolar Current (ACC), the Kuroshio Current, the Agulhas Current and the Gulf Stream. 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https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Concept current https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Concept overturning https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Concept steady state https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Concept surface https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Concept theory https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Concept thermocline https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Concept trend https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#FieldOfResearch earth sciences https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ 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https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Phrase Arons theory https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Phrase currents in the abyss https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Phrase meridional overturning https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Phrase steady state ocean circulation https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Phrase thermocline theory https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Sentence The simulated ocean circulation contains many of the observed currents in the world, like the Antarctic Circumpolar Current (ACC) the Kuroshio Current, the https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Sentence The thermally driven large-scale ocean circulation is studied. https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://w3id.org/ro/earth-science#Sentence We obtain a steady state ocean circulation by running the time-dependent, nonlinear model to equi- librium using restoring boundary conditions on surface temperature. https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/ro#ResearchObject https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/roevo#LiveRO https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/Dataset https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://w3id.org/ro/earth-science#DataResearchObject https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#DataResearchObject https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ https://w3id.org/contentdesc#Domain hydrography https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ https://w3id.org/contentdesc#Place Agulhas https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ https://www.w3.org/ns/iana/link-relations/relation#cite-as Liv Denstad. "Todays bathymetry with no wall using MITgcm." ROHub. 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(2015).Todays bathymetry with no wall using MITgcm [Data set]. Norstore. https://doi.org/10.11582/2015.00032 https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://purl.org/dc/terms/rightsHolder Joseph Henry Lacasce https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://purl.org/dc/terms/type Model https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://schema.org/author mailto:georgehadib@gmail.com https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://schema.org/contentUrl https://archive.sigma2.no/pages/public/datasetDetail.jsf?id=10.11582/2015.00032 https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://schema.org/creator mailto:georgehadib@gmail.com https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://schema.org/dateCreated 2015-10-21 00:00:00 https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://schema.org/dateModified 2022-03-22 01:18:38.407341+00:00 https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://schema.org/description The thermally driven large-scale ocean circulation is studied. We obtain a steady state ocean circulation by running the time-dependent, nonlinear model to equi- librium using restoring boundary conditions on surface temperature. This is simulated by MITgcm using a 2◦ × 2◦ spherical polar grid. We examine how this circulation relates to theories of the surface - and the abyssal circulation. These theories include the linear thermocline theory and Stommel and Arons theory. An important factor in returning the deep water to the surface, is the diapycnal mixing. Why this is important will be discussed. The reasons why and where the deep water upwells, are well debated. We find that positive vertical velocity mainly occurs at the western boundaries, where both the currents in the abyss and at the surface are strong. The simulated ocean circulation contains many of the observed currents in the world, like the Antarctic Circumpolar Current (ACC), the Kuroshio Current, the Agulhas Current and the Gulf Stream. In addition, the meridional overturning has a realistic strength. https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://schema.org/license https://choosealicense.com/no-permission/ https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://schema.org/name Todays bathymetry with no wall using MITgcm https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://schema.org/sdDatePublished 2015-10-21 00:00:00 https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/wf4ever#Dataset https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/wf4ever#Resource https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/MediaObject https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/resources/79c67dd7-ef10-4959-b55a-2956f9780f7f https://schema.org/maintainer Joseph Henry Lacasce https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ro-crate-metadata.json http://purl.org/dc/terms/conformsTo https://w3id.org/ro/crate/1.1 https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ro-crate-metadata.json http://schema.org/about https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ro-crate-metadata.json http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/CreativeWork mailto:georgehadib@gmail.com http://schema.org/name Geo H. mailto:georgehadib@gmail.com http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://xmlns.com/foaf/0.1/Agent mailto:liv.denstad@rohub.com http://schema.org/email liv.denstad@rohub.com mailto:liv.denstad@rohub.com http://schema.org/name Liv Denstad mailto:liv.denstad@rohub.com http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://xmlns.com/foaf/0.1/Agent https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I/provenance https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I/assertion http://www.w3.org/ns/prov#wasDerivedFrom https://api.rohub.org/api/ros/0e0d1f22-1bcc-494a-91fc-08a9612777fb/crate/download/ro-crate-metadata.json https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I/pubinfo https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I http://purl.org/dc/terms/created 2026-03-03T16:16:03.736+01:00 https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I http://purl.org/dc/terms/creator https://w3id.org/kpxl/gen/terms/RoCrateBot https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I http://purl.org/nanopub/x/introduces https://w3id.org/ro-id/0e0d1f22-1bcc-494a-91fc-08a9612777fb/ https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/nanopub/x/RoCrateNanopub https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I http://www.w3.org/2000/01/rdf-schema#label Todays bathymetry with no wall using MITgcm https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I/sig http://purl.org/nanopub/x/hasAlgorithm RSA https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I/sig http://purl.org/nanopub/x/hasPublicKey MIIBIjANBgkqhkiG9w0BAQEFAAOCAQ8AMIIBCgKCAQEAxszSDYX5tuCSkP7UiCtftYPFNQVTjgNu0I5fwdML2DLRDlp0xzmsQXRk8oHuvwGvG1aMjj6cpUqO+0rz2Sg/wvHOgUpkRH8VJXvmlkhafMLCMtUtk5JIx7e+fkzCby+fnmD7kMkGLrT+OaExWwEDmNlCAt0TPKcHSdwsjso2isXjtAsGevyCMke8ufnFYpjs746JES1eNzVnHnn2Kp/lqcm60GM+J8dLgRZp7fX0anW098xhKym6+xXFzqeju0vYRIHBPerv+r7skWxwk+a7Sd8msqVeYEv6NTqnyWvyWb6Yh8cvj04N6qm/T6C5FUPLQhzSaQgMVMU6yLqjPuu9DwIDAQAB https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I/sig http://purl.org/nanopub/x/hasSignature vGlVSRsDkNhXgwy2FgBz2lbX7EwHLw/VmSr1beGwJnT9ls+keVKduZrrhblMd7KlFjsX3uWJCyd3WKDp2MJ/Tr3UO2LpQo1tVHiDB0gXT0Y7ry9huOFgoGav1ul4U8x1+Vz2EJ2D16XMNCg793XngNes3C8e35prXUJiiVbr53QDbIJfwEI/RSuffOnNQHCkO1S0iQF/ACjbMq6DNEsgMtbmRX5ILrajOde39FmVXVdvCuQxHJM3bYssmyMpGDZ8CzkEjWuMVRwpN+Pj7HwusRSw2+9Yo5TGll1tYxYrcUIEUFNsif62lP1rBD6vZMWcHEQ77Ywg0sxqMgqZCVoIug== https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I/sig http://purl.org/nanopub/x/hasSignatureTarget https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I https://w3id.org/np/RAr7nwP_wirLxqF95Z4rq8kI1megLQKaUm3k6L3q4vJ-I/sig http://purl.org/nanopub/x/signedBy https://w3id.org/kpxl/gen/terms/RoCrateBot