{"@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/1360004236558883584.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1175/jcli-d-15-0908.1"}},{"identifier":{"@type":"URI","@value":"http://journals.ametsoc.org/jcli/article-pdf/30/10/3473/4676048/jcli-d-15-0908_1.pdf"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Responses of Basal Melting of Antarctic Ice Shelves to the Climatic Forcing of the Last Glacial Maximum and CO2 Doubling"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n               <jats:p>Basal melting of the Antarctic ice shelves is an important factor in determining the stability of the Antarctic ice sheet. This study used the climatic outputs of an atmosphere–ocean general circulation model to force a circumpolar ocean model that resolves ice shelf cavity circulation to investigate the response of Antarctic ice shelf melting to different climatic conditions (i.e., to a doubling of CO2 and to the Last Glacial Maximum conditions). Sensitivity experiments were also conducted to investigate the roles of both surface atmospheric change and changes of oceanic lateral boundary conditions. It was found that the rate of change of basal melt due to climate warming is much greater (by an order of magnitude) than that due to cooling. This is mainly because the intrusion of warm water onto the continental shelves, linked to sea ice production and climate change, is crucial in determining the basal melt rate of many ice shelves. Sensitivity experiments showed that changes of atmospheric heat flux and ocean temperature are both important for warm and cold climates. The offshore wind change, together with atmospheric heat flux change, strongly affected the production of both sea ice and high-density water, preventing warmer water approaching the ice shelves under a colder climate. These results reflect the importance of both water mass formation in the Antarctic shelf seas and subsurface ocean temperature in understanding the long-term response to climate change of the melting of Antarctic ice shelves.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004236558883715","@type":"Researcher","foaf:name":[{"@value":"Takashi Obase"}],"jpcoar:affiliationName":[{"@value":"Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004236558883333","@type":"Researcher","foaf:name":[{"@value":"Ayako Abe-Ouchi"}],"jpcoar:affiliationName":[{"@value":"Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, and Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004236558883206","@type":"Researcher","foaf:name":[{"@value":"Kazuya Kusahara"}],"jpcoar:affiliationName":[{"@value":"Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Hobart, Tasmania, Australia, and Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420001326231484544","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40311641"},{"@type":"NRID","@value":"1000040311641"},{"@type":"NRID","@value":"9000018378170"},{"@type":"NRID","@value":"9000322680292"},{"@type":"NRID","@value":"9000284633441"},{"@type":"NRID","@value":"9000347079987"},{"@type":"NRID","@value":"9000256758070"},{"@type":"NRID","@value":"9000256758162"},{"@type":"NRID","@value":"9000009889619"},{"@type":"NRID","@value":"9000283905041"},{"@type":"NRID","@value":"9000318581005"},{"@type":"NRID","@value":"9000270166579"},{"@type":"NRID","@value":"9000270166581"},{"@type":"NRID","@value":"9000257827866"},{"@type":"NRID","@value":"9000257768170"},{"@type":"NRID","@value":"9000002647436"},{"@type":"NRID","@value":"9000356912592"},{"@type":"NRID","@value":"9000299562079"},{"@type":"NRID","@value":"9000241122162"},{"@type":"NRID","@value":"9000257768296"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/hiroyasu.hasumi"}],"foaf:name":[{"@value":"Hiroyasu Hasumi"}],"jpcoar:affiliationName":[{"@value":"Atmosphere and Ocean Research Institute, University of Tokyo, Kashiwa, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004236558883344","@type":"Researcher","foaf:name":[{"@value":"Rumi Ohgaito"}],"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":"2017-04-19","prism:volume":"30","prism:number":"10","prism:startingPage":"3473","prism:endingPage":"3497"},"reviewed":"false","dc:rights":["http://www.ametsoc.org/PUBSReuseLicenses"],"url":[{"@id":"http://journals.ametsoc.org/jcli/article-pdf/30/10/3473/4676048/jcli-d-15-0908_1.pdf"}],"createdAt":"2017-02-13","modifiedAt":"2020-12-07","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=290","dc:title":"290"},{"@id":"https://cir.nii.ac.jp/all?q=CO2","dc:title":"CO2"},{"@id":"https://cir.nii.ac.jp/all?q=basal%20melting","dc:title":"basal melting"},{"@id":"https://cir.nii.ac.jp/all?q=Antarctic%20ice%20shelf","dc:title":"Antarctic ice shelf"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781825216768","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H02131"},{"@type":"JGN","@value":"JP15H02131"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H02131/"}],"notation":[{"@language":"ja","@value":"南大洋における乱流ホットスポットの定量化とその深層海洋大循環モデルへの組み込み"},{"@language":"en","@value":"Quantification of mixing hotspots in the Southern Ocean for accurate modeling of the global overturning circulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781833859072","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H05825"},{"@type":"JGN","@value":"JP15H05825"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-15H05825/"}],"notation":[{"@language":"ja","@value":"鉛直混合を取り入れた海洋循環・物質循環・気候モデル開発と影響評価"},{"@language":"en","@value":"Model development and impact assessment for ocea circulation, marine material cycles and climate by incorporating the effect of oceanic 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