{"@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/1363951793607017472.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1175/2009jcli3466.1"}},{"identifier":{"@type":"URI","@value":"http://journals.ametsoc.org/jcli/article-pdf/23/9/2418/3970719/2009jcli3466_1.pdf"}}],"dc:title":[{"@value":"Probing the Fast and Slow Components of Global Warming by Returning Abruptly to Preindustrial Forcing"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n               <jats:p>The fast and slow components of global warming in a comprehensive climate model are isolated by examining the response to an instantaneous return to preindustrial forcing. The response is characterized by an initial fast exponential decay with an e-folding time smaller than 5 yr, leaving behind a remnant that evolves more slowly. The slow component is estimated to be small at present, as measured by the global mean near-surface air temperature, and, in the model examined, grows to 0.4°C by 2100 in the A1B scenario from the Special Report on Emissions Scenarios (SRES), and then to 1.4°C by 2300 if one holds radiative forcing fixed after 2100. The dominance of the fast component at present is supported by examining the response to an instantaneous doubling of CO2 and by the excellent fit to the model’s ensemble mean twentieth-century evolution with a simple one-box model with no long times scales.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383951793607017474","@type":"Researcher","foaf:name":[{"@value":"Isaac M. Held"}],"jpcoar:affiliationName":[{"@value":"NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1383951793607017477","@type":"Researcher","foaf:name":[{"@value":"Michael Winton"}],"jpcoar:affiliationName":[{"@value":"NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1383951793607017476","@type":"Researcher","foaf:name":[{"@value":"Ken Takahashi"}],"jpcoar:affiliationName":[{"@value":"Instituto Geofisico del Peru, Lima, Peru"}]},{"@id":"https://cir.nii.ac.jp/crid/1383951793607017472","@type":"Researcher","foaf:name":[{"@value":"Thomas Delworth"}],"jpcoar:affiliationName":[{"@value":"NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1383951793607017475","@type":"Researcher","foaf:name":[{"@value":"Fanrong Zeng"}],"jpcoar:affiliationName":[{"@value":"NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey"}]},{"@id":"https://cir.nii.ac.jp/crid/1383951793607017473","@type":"Researcher","foaf:name":[{"@value":"Geoffrey K. Vallis"}],"jpcoar:affiliationName":[{"@value":"Atmospheric and Oceanic Sciences Program, Princeton University, Princeton, New Jersey"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"15200442"},{"@type":"PISSN","@value":"08948755"}],"prism:publicationName":[{"@value":"Journal of Climate"}],"dc:publisher":[{"@value":"American Meteorological Society"}],"prism:publicationDate":"2010-05-01","prism:volume":"23","prism:number":"9","prism:startingPage":"2418","prism:endingPage":"2427"},"reviewed":"false","url":[{"@id":"http://journals.ametsoc.org/jcli/article-pdf/23/9/2418/3970719/2009jcli3466_1.pdf"}],"createdAt":"2010-01-12","modifiedAt":"2020-12-07","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050589221516424448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Anthropogenic Influence on Extremes and Risk Hotspots"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021389797664768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A new conceptual model of global ocean heat uptake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181173607552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fast and slow timescales in the tropical low-cloud response to increasing CO2 in two climate models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656526612608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"What Caused the Global Surface Warming Hiatus of 1998–2013?"}]},{"@id":"https://cir.nii.ac.jp/crid/1390006231374131072","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Climate Econometric Analysis of Energy Balance Models:Cointegrating Relations Revisited"},{"@language":"ja","@value":"エネルギーバランスモデルの気候計量経済分析"},{"@value":"エネルギーバランスモデルの気候計量経済分析 : 共和分関係の再検討"},{"@language":"ja-Kana","@value":"エネルギーバランスモデル ノ キコウ ケイリョウ ケイザイ ブンセキ : キョウワ ブン カンケイ ノ サイケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681481577984","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Clouds and the Earth’s Radiant Energy System (CERES) Data Products for Climate Research"},{"@value":"Clouds and the Earth&rsquo;s Radiant Energy System (CERES) Data Products for Climate Research"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266842852864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A review of progress towards understanding the transient global mean surface temperature response to radiative perturbation"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1175/2009jcli3466.1"},{"@type":"CROSSREF","@value":"10.1186/s40645-016-0096-3_references_DOI_DGxgRoLOq1HLBn409P7AH4mqyIU"},{"@type":"CROSSREF","@value":"10.1007/s00382-023-06989-z_references_DOI_DGxgRoLOq1HLBn409P7AH4mqyIU"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2015-048_references_DOI_DGxgRoLOq1HLBn409P7AH4mqyIU"},{"@type":"CROSSREF","@value":"10.1038/s41598-022-27220-9_references_DOI_DGxgRoLOq1HLBn409P7AH4mqyIU"},{"@type":"CROSSREF","@value":"10.1007/s00382-011-1178-y_references_DOI_DGxgRoLOq1HLBn409P7AH4mqyIU"},{"@type":"CROSSREF","@value":"10.1007/s40641-017-0063-0_references_DOI_DGxgRoLOq1HLBn409P7AH4mqyIU"},{"@type":"CROSSREF","@value":"10.2457/srs.50.271_references_DOI_DGxgRoLOq1HLBn409P7AH4mqyIU"}]}