{"@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/1363670320640613632.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016gb005447"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GB005447"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016GB005447"}}],"dc:title":[{"@value":"One possible uncertainty in CMIP5 projections of low‐oxygen water volume in the Eastern Tropical Pacific"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Using the results from nine Earth system models submitted to the Coupled Model Intercomparison Project Phase 5 (CMIP5), we identify the Eastern Tropical Pacific (ETP) as the region with the greatest uncertainty of future changes in oxygen‐deficient (<30 μ<jats:italic>M</jats:italic>) water volumes since different models variously project both positive and negative changes in the oxygen‐deficient volume and export flux there. We investigate the factors controlling future changes in oxygen‐deficient volume in the ETP with global warming using a single off‐line biogeochemical model. Oxygen budget analysis clarifies that the Equatorial Undercurrent (EUC) is the key mechanism controlling future variations in the oxygen‐deficient volume in the ETP in our model. From the outputs of all of the CMIP5 models and our model, we identify a significant negative relationship between changes in the EUC volume transport and the oxygen‐deficient water volume from the present to the end of the 21st century, which indicates that the response of the EUC to global warming leads to one possible uncertainty in future projections of oxygen‐deficient volume in the ETP.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320640613762","@type":"Researcher","foaf:name":[{"@value":"M. Shigemitsu"}],"jpcoar:affiliationName":[{"@value":"Faculty of Environmental Earth Science Hokkaido University  Sapporo Japan"},{"@value":"Global Chemical and Physical Oceanography Group, Research and Development Center for Global Change Japan Agency for Marine‐Earth Science and Technology  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320640613632","@type":"Researcher","foaf:name":[{"@value":"A. Yamamoto"}],"jpcoar:affiliationName":[{"@value":"Atmosphere and Ocean Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320640613760","@type":"Researcher","foaf:name":[{"@value":"A. Oka"}],"jpcoar:affiliationName":[{"@value":"Atmosphere and Ocean Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320640613761","@type":"Researcher","foaf:name":[{"@value":"Y. Yamanaka"}],"jpcoar:affiliationName":[{"@value":"Faculty of Environmental Earth Science Hokkaido University  Sapporo Japan"}]}],"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":"2017-05","prism:volume":"31","prism:number":"5","prism:startingPage":"804","prism:endingPage":"820"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GB005447"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016GB005447"}],"createdAt":"2017-04-17","modifiedAt":"2023-09-17","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050585803064813824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Competing and accelerating effects of anthropogenic nutrient inputs on climate-driven changes in ocean carbon and oxygen cycles"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584341817125888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A nitrogen isoscape of phytoplankton in the western North Pacific created with a marine nitrogen isotope model"}]},{"@id":"https://cir.nii.ac.jp/crid/1361975846437609984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mechanisms of Future Changes in Equatorial Upwelling: CMIP5 Intermodel Analysis"}]},{"@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":"10.1002/2016gb005447"},{"@type":"OPENAIRE","@value":"doi_dedup___::02df07388020adc1a798d35de5a6e190"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00338-y_references_DOI_QGD2G3UivGLHmANrX18LdGGPbCm"},{"@type":"CROSSREF","@value":"10.1126/sciadv.abl9207_references_DOI_QGD2G3UivGLHmANrX18LdGGPbCm"},{"@type":"CROSSREF","@value":"10.3389/fmars.2024.1294608_references_DOI_QGD2G3UivGLHmANrX18LdGGPbCm"},{"@type":"CROSSREF","@value":"10.1175/jcli-d-19-0128.1_references_DOI_QGD2G3UivGLHmANrX18LdGGPbCm"}]}