{"@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/1360011142931369728.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1175/jcli-d-11-00152.1"}},{"identifier":{"@type":"URI","@value":"http://journals.ametsoc.org/jcli/article-pdf/25/6/2178/3991337/jcli-d-11-00152_1.pdf"}}],"dc:title":[{"@value":"Response of Upper Clouds in Global Warming Experiments Obtained Using a Global Nonhydrostatic Model with Explicit Cloud Processes"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Using a global nonhydrostatic model with explicit cloud processes, upper-cloud changes are investigated by comparing the present climate condition under the perpetual July setting and the global warming condition, in which the sea surface temperature (SST) is raised by 2°. The sensitivity of the upper-cloud cover and the ice water path (IWP) are investigated through a set of experiments. The responses of convective mass flux and convective areas are also examined, together with those of the large-scale subsidence and relative humidity in the subtropics. The responses of the IWP and the upper-cloud cover are found to be opposite; that is, as the SST increases, the IWP averaged over the tropics decreases, whereas the upper-cloud cover in the tropics increases. To clarify the IWP response, a simple conceptual model is constructed. The model consists of three columns of deep convective core, anvil, and environmental subsidence regions. The vertical profiles of hydrometers are predicted with cloud microphysics processes and kinematically prescribed circulation. The reduction in convective mass flux is found to be a primary factor in the decrease of the IWP under the global warming condition. Even when a different and more comprehensive cloud microphysics scheme is used, the reduction in the IWP due to the mass flux change is also confirmed.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011142931369728","@type":"Researcher","foaf:name":[{"@value":"Masaki Satoh"}],"jpcoar:affiliationName":[{"@value":"Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, and Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142931369732","@type":"Researcher","foaf:name":[{"@value":"Shin-ichi Iga"}],"jpcoar:affiliationName":[{"@value":"RIKEN Advanced Institute for Computational Science, Hyogo, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142931369730","@type":"Researcher","foaf:name":[{"@value":"Hirofumi Tomita"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine-Earth Science and Technology, Yokohama, and RIKEN Advanced Institute for Computational Science, Hyogo, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142931369729","@type":"Researcher","foaf:name":[{"@value":"Yoko Tsushima"}],"jpcoar:affiliationName":[{"@value":"Met Office Hadley Centre, Exeter, United Kingdom"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142931369731","@type":"Researcher","foaf:name":[{"@value":"Akira T. Noda"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine-Earth Science and Technology, Yokohama, 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":"2012-03-14","prism:volume":"25","prism:number":"6","prism:startingPage":"2178","prism:endingPage":"2191"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://journals.ametsoc.org/jcli/article-pdf/25/6/2178/3991337/jcli-d-11-00152_1.pdf"}],"createdAt":"2011-10-11","modifiedAt":"2024-04-13","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/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/1390001206504762880","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Constraint on Future Change in Global Frequency of Tropical Cyclones due to Global Warming"},{"@value":"NOTES AND CORRESPONDENCE : Constraint on Future Change in Global Frequency of Tropical Cyclones due to Global Warming"}]},{"@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"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842089639168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Non-hydrostatic Icosahedral Atmospheric Model : description and development"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1175/jcli-d-11-00152.1"},{"@type":"OPENAIRE","@value":"doi_dedup___::4a02f4d79b90d17d53f4d71e29cd0b30"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2015-025_references_DOI_6Q3RUjqK09zBs22gZWa2yAF3ckX"},{"@type":"CROSSREF","@value":"10.1029/2021jd035223_references_DOI_6Q3RUjqK09zBs22gZWa2yAF3ckX"},{"@type":"CROSSREF","@value":"10.1029/2021gl093646_references_DOI_6Q3RUjqK09zBs22gZWa2yAF3ckX"},{"@type":"CROSSREF","@value":"10.1186/s40645-014-0018-1_references_DOI_6Q3RUjqK09zBs22gZWa2yAF3ckX"},{"@type":"CROSSREF","@value":"10.1186/s40645-017-0127-8_references_DOI_6Q3RUjqK09zBs22gZWa2yAF3ckX"},{"@type":"CROSSREF","@value":"10.1175/jcli-d-21-0150.1_references_DOI_6Q3RUjqK09zBs22gZWa2yAF3ckX"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2020-024_references_DOI_6Q3RUjqK09zBs22gZWa2yAF3ckX"}]}