{"@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/1364233270979192192.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2005gb002489"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005GB002489"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005GB002489"}}],"dc:title":[{"@value":"A factorial analysis of the marine carbon cycle and ocean circulation controls on atmospheric CO<sub>2</sub>"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>A factorial experiment with a new Earth system model of intermediate complexity is used to assess the sensitivity of atmospheric CO<jats:sub>2</jats:sub> to organic, carbonate and solubility pumps, ocean circulation state, and climate feedback. An analysis of variance of the results reveals that the organic, carbonate, and solubility pumps act multiplicatively and account for 94% of the variance of atmospheric CO<jats:sub>2</jats:sub>. The organic pump explains 63% (89 ppm), the solubility pump 24% (55 ppm), the carbonate pump 6% (28 ppm), and ocean circulation 0.3% (12 ppm) of the variance. Removing all pumps increases atmospheric CO<jats:sub>2</jats:sub> from 278 to 525 ppm. Including interactions with all the pumps increases the effects of ocean circulation from 12 to 56 ppm. However, the ocean circulation states used are unlikely to span the full range of possible states. Changes in Pacific circulation have more effect on atmospheric CO<jats:sub>2</jats:sub> than Atlantic circulation.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1384233270979192197","@type":"Researcher","foaf:name":[{"@value":"David R. Cameron"}],"jpcoar:affiliationName":[{"@value":"Centre for Ecology and Hydrology, Bush Estate  Penicuik UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233270979192193","@type":"Researcher","foaf:name":[{"@value":"Timothy M. Lenton"}],"jpcoar:affiliationName":[{"@value":"School of Environmental Sciences University of East Anglia  Norwich UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233270979192192","@type":"Researcher","foaf:name":[{"@value":"Andy J. Ridgwell"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Ocean Sciences University of British Columbia  Vancouver, British Columbia Canada"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233270979192196","@type":"Researcher","foaf:name":[{"@value":"John G. Shepherd"}],"jpcoar:affiliationName":[{"@value":"National Oceanography Centre  Southampton UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233270979192195","@type":"Researcher","foaf:name":[{"@value":"Robert Marsh"}],"jpcoar:affiliationName":[{"@value":"National Oceanography Centre  Southampton UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233270979192194","@type":"Researcher","foaf:name":[{"@value":"Andrew Yool"}],"jpcoar:affiliationName":[{"@value":"National Oceanography Centre  Southampton UK"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"08866236"},{"@type":"EISSN","@value":"19449224"}],"prism:publicationName":[{"@value":"Global Biogeochemical Cycles"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2005-12","prism:volume":"19","prism:number":"4"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005GB002489"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005GB002489"}],"createdAt":"2005-12-29","modifiedAt":"2023-10-12","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360022306718344064","@type":"Article","resourceType":"preprint","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Glacial marine carbon cycle sensitivities to Atlantic ocean circulation reorganization  by coupled climate model simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565171070598784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quantifying the ocean's role in glacial CO\n                    <sub>2</sub>\n                    reductions"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417119877760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ocean carbon pump decomposition and its application to CMIP5 earth system model simulations"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2005gb002489"},{"@type":"CROSSREF","@value":"10.5194/cpd-7-1261-2011_references_DOI_1hixhWAxdmnLgEPRNslVaKznYf6"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00338-y_references_DOI_1hixhWAxdmnLgEPRNslVaKznYf6"},{"@type":"CROSSREF","@value":"10.5194/cp-8-545-2012_references_DOI_1hixhWAxdmnLgEPRNslVaKznYf6"}]}