{"@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/1361699995052619008.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1175/jcli-d-15-0668.1"}},{"identifier":{"@type":"URI","@value":"http://journals.ametsoc.org/jcli/article-pdf/29/16/5949/4071516/jcli-d-15-0668_1.pdf"}}],"dc:title":[{"@value":"High Cloud Responses to Global Warming Simulated by Two Different Cloud Microphysics Schemes Implemented in the Nonhydrostatic Icosahedral Atmospheric Model (NICAM)"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n               <jats:p>This study examines cloud responses to global warming using a global nonhydrostatic model with two different cloud microphysics schemes. The cloud microphysics schemes tested here are the single- and double-moment schemes with six water categories: these schemes are referred to as NSW6 and NDW6, respectively. Simulations of one year for NSW6 and one boreal summer for NDW6 are performed using the nonhydrostatic icosahedral atmospheric model with a mesh size of approximately 14 km. NSW6 and NDW6 exhibit similar changes in the visible cloud fraction under conditions of global warming. The longwave (LW) cloud radiative feedbacks in NSW6 and NDW6 are within the upper half of the phase 5 of the Coupled Model Intercomparison Project (CMIP5)–Cloud Feedback Model Intercomparison Project 2 (CFMIP2) range. The LW cloud radiative feedbacks are mainly attributed to cirrus clouds, which prevail more in the tropics under global warming conditions. For NDW6, the LW cloud radiative feedbacks from cirrus clouds also extend to midlatitudes. The changes in cirrus clouds and their effects on LW cloud radiative forcing (LWCRF) are assessed based on changes in the effective radii of ice hydrometeors () and the cloud fraction. It was determined that an increase in has a nonnegligible impact on LWCRF compared with an increase in cloud fraction.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380003444163981952","@type":"Researcher","personIdentifier":[{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/yingwenchen"}],"foaf:name":[{"@value":"Ying-Wen Chen"}]},{"@id":"https://cir.nii.ac.jp/crid/1420564276176432896","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60599968"},{"@type":"NRID","@value":"1000060599968"},{"@type":"NRID","@value":"9000412099072"},{"@type":"NRID","@value":"9000410513236"},{"@type":"NRID","@value":"9000290819259"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/cloud"}],"foaf:name":[{"@value":"Tatsuya Seiki"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995052619013","@type":"Researcher","foaf:name":[{"@value":"Chihiro Kodama"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995052619011","@type":"Researcher","foaf:name":[{"@value":"Masaki Satoh"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine-Earth Science and Technology, Yokohama, and Atmosphere and Ocean Research Institute, The University of Tokyo, Tokyo, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995052619010","@type":"Researcher","foaf:name":[{"@value":"Akira T. Noda"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995052619012","@type":"Researcher","foaf:name":[{"@value":"Yohei Yamada"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine-Earth Science and Technology, Yokohama, and Atmosphere and Ocean Research Institute, The University of Tokyo, Tokyo, Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"08948755"},{"@type":"EISSN","@value":"15200442"}],"prism:publicationName":[{"@value":"Journal of Climate"}],"dc:publisher":[{"@value":"American Meteorological Society"}],"prism:publicationDate":"2016-08-04","prism:volume":"29","prism:number":"16","prism:startingPage":"5949","prism:endingPage":"5964"},"reviewed":"false","url":[{"@id":"http://journals.ametsoc.org/jcli/article-pdf/29/16/5949/4071516/jcli-d-15-0668_1.pdf"}],"createdAt":"2016-05-19","modifiedAt":"2020-12-07","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570393522816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Outcomes and challenges of global high-resolution non-hydrostatic atmospheric simulations using the K computer"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142459319936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Nonhydrostatic ICosahedral Atmospheric Model for CMIP6 HighResMIP simulations (NICAM16-S): experimental design, model description, and impacts of model updates"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282208105344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Improved Representation of Low‐Level Mixed‐Phase Clouds in a Global Cloud‐System‐Resolving Simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282443448576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Importance of Pressure Changes in High Cloud Area Feedback Due to Global Warming"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302866840956288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Projection of High Clouds and the Link to Ice Hydrometeors: An Approach Using Long-Term Global Cloud System–Resolving Simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118681884800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Clouds and Convective Self‐Aggregation in a Multimodel Ensemble of Radiative‐Convective Equilibrium Simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412896484185728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fixed Anvil Temperature Feedback: Positive, Zero, or Negative?"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288145100928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"JAMSTEC Model Intercomparision Project (JMIP)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390285300156042112","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Precipitation Efficiency and its Role in Cloud-Radiative Feedbacks to Climate Variability"},{"@language":"ja","@value":"降水効率および気候変動に対する雲放射フィードバックにおけるその役割"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1175/jcli-d-15-0668.1"},{"@type":"OPENAIRE","@value":"doi_dedup___::126a70ed1ae3c0678f93e2acd67a0020"},{"@type":"CROSSREF","@value":"10.5194/gmd-14-795-2021_references_DOI_ZM8Svbented2Ac38g7aUVvBuW8o"},{"@type":"CROSSREF","@value":"10.1029/2021jd035223_references_DOI_ZM8Svbented2Ac38g7aUVvBuW8o"},{"@type":"CROSSREF","@value":"10.1029/2021gl093646_references_DOI_ZM8Svbented2Ac38g7aUVvBuW8o"},{"@type":"CROSSREF","@value":"10.1186/s40645-017-0127-8_references_DOI_ZM8Svbented2Ac38g7aUVvBuW8o"},{"@type":"CROSSREF","@value":"10.1175/jcli-d-21-0150.1_references_DOI_ZM8Svbented2Ac38g7aUVvBuW8o"},{"@type":"CROSSREF","@value":"10.1029/2020ms002138_references_DOI_ZM8Svbented2Ac38g7aUVvBuW8o"},{"@type":"CROSSREF","@value":"10.5918/jamstecr.28.5_references_DOI_ZM8Svbented2Ac38g7aUVvBuW8o"},{"@type":"CROSSREF","@value":"10.1175/jcli-d-19-0108.1_references_DOI_ZM8Svbented2Ac38g7aUVvBuW8o"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2020-024_references_DOI_ZM8Svbented2Ac38g7aUVvBuW8o"}]}