{"@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/1362825896161582848.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1175/jcli-d-12-00150.1"}},{"identifier":{"@type":"URI","@value":"https://journals.ametsoc.org/view/journals/clim/26/7/jcli-d-12-00150.1.xml"}},{"identifier":{"@type":"URI","@value":"http://journals.ametsoc.org/jcli/article-pdf/26/7/2247/4004750/jcli-d-12-00150_1.pdf"}},{"identifier":{"@type":"URI","@value":"https://journals.ametsoc.org/downloadpdf/journals/clim/26/7/jcli-d-12-00150.1.xml"}}],"dc:title":[{"@value":"GFDL’s ESM2 Global Coupled Climate–Carbon Earth System Models. Part II: Carbon System Formulation and Baseline Simulation Characteristics*"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n<jats:p>The authors describe carbon system formulation and simulation characteristics of two new global coupled carbon–climate Earth System Models (ESM), ESM2M and ESM2G. These models demonstrate good climate fidelity as described in part I of this study while incorporating explicit and consistent carbon dynamics. The two models differ almost exclusively in the physical ocean component; ESM2M uses the Modular Ocean Model version 4.1 with vertical pressure layers, whereas ESM2G uses generalized ocean layer dynamics with a bulk mixed layer and interior isopycnal layers. On land, both ESMs include a revised land model to simulate competitive vegetation distributions and functioning, including carbon cycling among vegetation, soil, and atmosphere. In the ocean, both models include new biogeochemical algorithms including phytoplankton functional group dynamics with flexible stoichiometry. Preindustrial simulations are spun up to give stable, realistic carbon cycle means and variability. Significant differences in simulation characteristics of these two models are described. Because of differences in oceanic ventilation rates, ESM2M has a stronger biological carbon pump but weaker northward implied atmospheric CO<jats:sub>2</jats:sub> transport than ESM2G. The major advantages of ESM2G over ESM2M are improved representation of surface chlorophyll in the Atlantic and Indian Oceans and thermocline nutrients and oxygen in the North Pacific. Improved tree mortality parameters in ESM2G produced more realistic carbon accumulation in vegetation pools. The major advantages of ESM2M over ESM2G are reduced nutrient and oxygen biases in the southern and tropical oceans.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825896161582723","@type":"Researcher","foaf:name":[{"@value":"John P. Dunne"}],"jpcoar:affiliationName":[{"@value":"+ National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582850","@type":"Researcher","foaf:name":[{"@value":"Jasmin G. John"}],"jpcoar:affiliationName":[{"@value":"+ National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582861","@type":"Researcher","foaf:name":[{"@value":"Elena Shevliakova"}],"jpcoar:affiliationName":[{"@value":"# Department of Ecology and Evolutionary Biology, Princeton University, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582856","@type":"Researcher","foaf:name":[{"@value":"Ronald J. Stouffer"}],"jpcoar:affiliationName":[{"@value":"+ National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582857","@type":"Researcher","foaf:name":[{"@value":"John P. Krasting"}],"jpcoar:affiliationName":[{"@value":"@ National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, and High Performance Technologies Group, DRC/GFDL, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582851","@type":"Researcher","foaf:name":[{"@value":"Sergey L. Malyshev"}],"jpcoar:affiliationName":[{"@value":"# Department of Ecology and Evolutionary Biology, Princeton University, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582854","@type":"Researcher","foaf:name":[{"@value":"P. C. D. Milly"}],"jpcoar:affiliationName":[{"@value":"& U.S. Geological Survey, and National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582852","@type":"Researcher","foaf:name":[{"@value":"Lori T. Sentman"}],"jpcoar:affiliationName":[{"@value":"+ National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582849","@type":"Researcher","foaf:name":[{"@value":"Alistair J. Adcroft"}],"jpcoar:affiliationName":[{"@value":"** Program in Atmospheric and Oceanic Sciences, Princeton University, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582858","@type":"Researcher","foaf:name":[{"@value":"William Cooke"}],"jpcoar:affiliationName":[{"@value":"++ High Performance Technologies Group, DRC/GFDL, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582720","@type":"Researcher","foaf:name":[{"@value":"Krista A. Dunne"}],"jpcoar:affiliationName":[{"@value":"& U.S. Geological Survey, and National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582722","@type":"Researcher","foaf:name":[{"@value":"Stephen M. Griffies"}],"jpcoar:affiliationName":[{"@value":"+ National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582855","@type":"Researcher","foaf:name":[{"@value":"Robert W. Hallberg"}],"jpcoar:affiliationName":[{"@value":"+ National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582860","@type":"Researcher","foaf:name":[{"@value":"Matthew J. Harrison"}],"jpcoar:affiliationName":[{"@value":"+ National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582721","@type":"Researcher","foaf:name":[{"@value":"Hiram Levy"}],"jpcoar:affiliationName":[{"@value":"+ National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582853","@type":"Researcher","foaf:name":[{"@value":"Andrew T. Wittenberg"}],"jpcoar:affiliationName":[{"@value":"+ National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582859","@type":"Researcher","foaf:name":[{"@value":"Peter J. Phillips"}],"jpcoar:affiliationName":[{"@value":"+ National Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896161582848","@type":"Researcher","foaf:name":[{"@value":"Niki Zadeh"}],"jpcoar:affiliationName":[{"@value":"++ High Performance Technologies Group, DRC/GFDL, Princeton, New Jersey"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"08948755"},{"@type":"EISSN","@value":"15200442"}],"prism:publicationName":[{"@value":"Journal of Climate"}],"dc:publisher":[{"@value":"American Meteorological Society"}],"prism:publicationDate":"2013-04-01","prism:volume":"26","prism:number":"7","prism:startingPage":"2247","prism:endingPage":"2267"},"reviewed":"false","url":[{"@id":"https://journals.ametsoc.org/view/journals/clim/26/7/jcli-d-12-00150.1.xml"},{"@id":"http://journals.ametsoc.org/jcli/article-pdf/26/7/2247/4004750/jcli-d-12-00150_1.pdf"},{"@id":"https://journals.ametsoc.org/downloadpdf/journals/clim/26/7/jcli-d-12-00150.1.xml"}],"createdAt":"2012-10-12","modifiedAt":"2022-03-04","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004229803475456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"On the Southern Ocean CO<sub>2</sub> uptake and the role of the biological carbon pump in the 21st century"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004240191795840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Drivers and uncertainties of future global marine primary production in marine ecosystem models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283689326283264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"How well do global ocean biogeochemistry models simulate dissolved iron distributions?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092475646336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Excessive positive response of model‐simulated land net primary production to climate changes over circumboreal forests"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567638367488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Is there warming in the pipeline? 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