{"@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/1360013168739147136.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/s00382-021-06056-5"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1007/s00382-021-06056-5.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1007/s00382-021-06056-5/fulltext.html"}},{"identifier":{"@type":"DOI","@value":"10.21203/rs.3.rs-168070/v1"}},{"identifier":{"@type":"URI","@value":"https://www.researchsquare.com/article/rs-168070/v1"}},{"identifier":{"@type":"URI","@value":"https://www.researchsquare.com/article/rs-168070/v1.html"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Response of convective systems to the orbital forcing of the last interglacial in a global nonhydrostatic atmospheric model with and without a convective parameterization"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n                  <jats:p>Nonhydrostatic Icosahedral Atmospheric Model (NICAM) coupled with a slab ocean model was applied to a paleoclimate research for the first time. The model was run at a horizontal resolution of 56 km with and without a convective parameterization, given the orbital parameters of the last interglacial (127,000 years before present). The simulated climatological mean-states are qualitatively similar to those in previous studies reinforcing their robustness, however, the resolution of this model enables to represent the narrow precipitation band along the southern edge of the Tibetan Plateau. A particular focus was given to convectively coupled disturbances in our analysis. The simulated results show a greater signal of the Madden–Julian Oscillation and weakening of the moist Kelvin waves. Although the model's representation of the boreal summer intraseasonal oscillation in the present-day simulations is not satisfactory, a significant enhancement of its signal is found in the counterpart of the last interglacial. The density of the tropical cyclones decreases over the western north Pacific, north Atlantic and increases over the south Indian Ocean and south Atlantic. The model's performance is generally better when the convective parameterization is used, but the tropical cyclones are better represented without the convective parameterization. Additional simulations using the low-resolution topography reveals that the better representation of the Tibetan Plateau enhances the boreal summer Asian monsoon and its impact is similar and comparable to that of the orbital parameters over the south Asia and the Indian Ocean.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1030003658734173184","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20419146"},{"@type":"NRID","@value":"1000020419146"},{"@type":"NRID","@value":"9000001341445"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/4G1QiM47b4"}],"foaf:name":[{"@value":"Minoru Chikira"}]},{"@id":"https://cir.nii.ac.jp/crid/1380013168739146914","@type":"Researcher","foaf:name":[{"@value":"Yohei Yamada"}]},{"@id":"https://cir.nii.ac.jp/crid/1380013168739146913","@type":"Researcher","foaf:name":[{"@value":"Ayako Abe-Ouchi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380013168739146881","@type":"Researcher","foaf:name":[{"@value":"Masaki Satoh"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"09307575"},{"@type":"EISSN","@value":"14320894"}],"prism:publicationName":[{"@value":"Climate Dynamics"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2022-01-01","prism:volume":"59","prism:number":"5-6","prism:startingPage":"1617","prism:endingPage":"1648"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/4.0","https://creativecommons.org/licenses/by/4.0"],"url":[{"@id":"https://link.springer.com/content/pdf/10.1007/s00382-021-06056-5.pdf"},{"@id":"https://link.springer.com/article/10.1007/s00382-021-06056-5/fulltext.html"},{"@id":"https://www.researchsquare.com/article/rs-168070/v1"},{"@id":"https://www.researchsquare.com/article/rs-168070/v1.html"}],"createdAt":"2022-01-04","modifiedAt":"2022-08-11","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282256935981184","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"17H06104"},{"@type":"JGN","@value":"JP17H06104"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-17H06104/"}],"notation":[{"@language":"ja","@value":"過去の大規模な気候変動における氷床・海洋・大気の相互作用の解明"},{"@language":"en","@value":"Understanding the interaction between ice sheets, ocean and atmosphere under large scale climate changes of the past"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256994004480","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"19K03964"},{"@type":"JGN","@value":"JP19K03964"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-19K03964/"}],"notation":[{"@language":"ja","@value":"高解像度大気モデルで利用可能な積雲パラメタリゼーションの開発"},{"@language":"en","@value":"Development of cumulus parameterization available for high-resolution atmospheric model"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570393522816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"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/1360002216709789568","@type":"Article","resourceType":"学術雑誌論文(journal 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