{"@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/1390282680198452864.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/sola.2012-016"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/sola/8/0/8_2012-016/_pdf"}},{"identifier":{"@type":"NAID","@value":"130004448575"}}],"dc:title":[{"@language":"en","@value":"Downscaling of Snow Cover Changes in the Late 20th Century Using a Past Climate Simulation Method over Central Japan"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"We focus on the dramatic decrease in the snow cover on the Japan Sea side of Central Japan in the late 20th century. Using a regional climate model, a control experiment (CTL) was conducted, and it accurately simulated the dramatic decrease in maximum snow depth (SNDmax) between the 1980s and the 1990s. We then conducted a pseudo climate simulation (PCS) in the 1990s, which assumes the mean atmospheric fields in the 1990s and the perturbation from the mean atmospheric fields in the 1980s. The PCS method is expected to evaluate only the impacts of changes in the mean atmospheric fields on the snow cover changes. The PCS simulates the decreases in SNDmax over the coastal area, which are comparable to the changes simulated by the CTL. On the other hand, changes in SNDmax are negligible in the PCS over the mountainous area, where the slight increases in SNDmax are simulated by the CTL. Therefore, the changes in the mean atmospheric fields, especially, the mean temperature rise, are main factors of the snow cover decrease over the coastal area, while changes in both the mean atmospheric fields and the perturbation contribute to the snow cover changes over the mountainous area."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420845751137595520","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20537287"},{"@type":"NRID","@value":"1000020537287"},{"@type":"ORCID","@value":"0000-0003-4865-791X"},{"@type":"CINII_AUTHOR_ID","@value":"DA18141352"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA18141352#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA18141352"},{"@type":"NRID","@value":"9000386307408"},{"@type":"NRID","@value":"9000377397852"},{"@type":"NRID","@value":"9000399222109"},{"@type":"NRID","@value":"9000283593359"},{"@type":"NRID","@value":"9000001341210"},{"@type":"NRID","@value":"9000257827574"},{"@type":"NRID","@value":"9000402244048"},{"@type":"NRID","@value":"9000257768567"},{"@type":"NRID","@value":"9000283593422"},{"@type":"NRID","@value":"9000409326737"},{"@type":"NRID","@value":"9000258267921"},{"@type":"NRID","@value":"9000265248598"},{"@type":"NRID","@value":"9000347189771"},{"@type":"NRID","@value":"9000020045155"},{"@type":"NRID","@value":"9000377397857"},{"@type":"NRID","@value":"9000399763154"},{"@type":"NRID","@value":"9000402243991"},{"@type":"NRID","@value":"9000405666047"},{"@type":"NRID","@value":"9000257828078"},{"@type":"NRID","@value":"9000402243999"},{"@type":"NRID","@value":"9000391687023"},{"@type":"NRID","@value":"9000402248411"},{"@type":"NRID","@value":"9000257828200"},{"@type":"NRID","@value":"9000402593436"},{"@type":"NRID","@value":"9000411370440"},{"@type":"NRID","@value":"9000399936682"},{"@type":"NRID","@value":"9000241674253"},{"@type":"NRID","@value":"9000387897641"},{"@type":"NRID","@value":"9000402614863"},{"@type":"NRID","@value":"9000408426307"},{"@type":"NRID","@value":"9000402822848"},{"@type":"NRID","@value":"9000409646461"},{"@type":"NRID","@value":"9000375898440"},{"@type":"NRID","@value":"9000311066885"},{"@type":"NRID","@value":"9000411368559"},{"@type":"NRID","@value":"9000386399848"},{"@type":"NRID","@value":"9000311062251"},{"@type":"NRID","@value":"9000347189871"},{"@type":"NRID","@value":"9000293836686"},{"@type":"NRID","@value":"9000327098761"},{"@type":"NRID","@value":"9000283236641"},{"@type":"NRID","@value":"9000257828037"},{"@type":"NRID","@value":"9000399252239"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/kawasehiroaki"}],"foaf:name":[{"@language":"en","@value":"Kawase 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Impact of Global Warming on Snow Depth in Japan by the Pseudo-Global-Warming Method"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206506288256","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Defining Indices for the Extreme Snowfall Events and Analyzing their Trends in Northern Xinjiang, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679401086208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"日本における降雪深変動の地域性とその要因"},{"@language":"en","@value":"Regional Characteristics of Variation of Snowfall in Japan"},{"@language":"ja-Kana","@value":"ニホン ニ オケル コウセツシンヘンドウ ノ チイキセイ ト ソノ ヨウイン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680199922176","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Verification of the Performance of the Pseudo-Global-Warming Method for Future Climate Changes during 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