{"@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/1390282680199989376.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/sola.2013-006"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/sola/9/0/9_2013-006/_pdf"}},{"identifier":{"@type":"NAID","@value":"130004940971"}}],"dc:title":[{"@language":"en","@value":"Projection of Changes in Future Surface Wind around Japan Using a Non-hydrostatic Regional Climate Model"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Changes of a surface wind under the future climate condition in and around Japan were investigated by using a 5-km-mesh non-hydrostatic regional climate model (NHRCM05). In the present climate, monthly mean surface wind speeds are well reproduced by NHRCM05. Additionally, the NHRCM05 reproduces the seasonal change of mean surface wind speeds fairly well: the wind during the cold season is calculated to be stronger than that in the warm season.<br>Under the future climate, monthly mean surface wind speeds show little change. In the warm season, according to a 20-km-mesh atmospheric general circulation model (AGCM20), the Pacific anticyclone is projected to weaken near Japan, and the sea level pressure over the seas around the Philippine Islands is projected to rise, so the frequency of the westerly wind is projected to increase across Japan by NHRCM05.<br>During the cold season, according to NHRCM05, the wind speeds around Hokkaido are projected to increase a little value due to the decrease of the sea ice in the Sea of Okhotsk. Further, the frequency of southeasterly wind is projected to increase significantly. In the future, the Monsoon Index is projected to be lower than in the present climate by AGCM20, resulting in southeasterly wind inflow to Japan."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282680199989378","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000283593868"}],"foaf:name":[{"@language":"en","@value":"Hanafusa Mizuki"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282680199989377","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000283593869"}],"foaf:name":[{"@language":"en","@value":"Sasaki Hidetaka"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801204951296","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"10354474"},{"@type":"NRID","@value":"1000010354474"},{"@type":"NRID","@value":"9000386307414"},{"@type":"NRID","@value":"9000257828030"},{"@type":"NRID","@value":"9000363497675"},{"@type":"NRID","@value":"9000283593870"},{"@type":"NRID","@value":"9000363502197"},{"@type":"NRID","@value":"9000409863556"},{"@type":"NRID","@value":"9000402243996"},{"@type":"NRID","@value":"9000391687021"},{"@type":"NRID","@value":"9000404111096"},{"@type":"NRID","@value":"9000363499760"},{"@type":"NRID","@value":"9000402248408"},{"@type":"NRID","@value":"9000257768312"},{"@type":"NRID","@value":"9000402593433"},{"@type":"NRID","@value":"9000403426247"},{"@type":"NRID","@value":"9000411370444"},{"@type":"NRID","@value":"9000387897648"},{"@type":"NRID","@value":"9000392819697"},{"@type":"NRID","@value":"9000283593885"},{"@type":"NRID","@value":"9000405697409"},{"@type":"NRID","@value":"9000018916423"},{"@type":"NRID","@value":"9000402614865"},{"@type":"NRID","@value":"9000408426306"},{"@type":"NRID","@value":"9000375898433"},{"@type":"NRID","@value":"9000404665120"},{"@type":"NRID","@value":"9000392818816"},{"@type":"NRID","@value":"9000411368560"},{"@type":"NRID","@value":"9000311062253"},{"@type":"NRID","@value":"9000347189873"},{"@type":"NRID","@value":"9000293836681"},{"@type":"NRID","@value":"9000327098760"},{"@type":"NRID","@value":"9000257827936"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/handle0101391"}],"foaf:name":[{"@language":"en","@value":"Murata Akihiko"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282680199989379","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000283593871"}],"foaf:name":[{"@language":"en","@value":"Kurihara Kazuo"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"13496476"}],"prism:publicationName":[{"@language":"en","@value":"SOLA"},{"@language":"en","@value":"SOLA"}],"dc:publisher":[{"@language":"en","@value":"Meteorological Society of Japan"},{"@language":"ja","@value":"公益社団法人 日本気象学会"}],"prism:publicationDate":"2013","prism:volume":"9","prism:number":"0","prism:startingPage":"23","prism:endingPage":"26"},"reviewed":"false","url":[{"@id":"https://www.jstage.jst.go.jp/article/sola/9/0/9_2013-006/_pdf"}],"availableAt":"2013","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002218811534080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Future Change in Extratropical Cyclones Associated with Change in the Upper Troposphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520270398336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Will climate change impact on wind power development in the UK?"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368451219712","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Potential climate change impact on wind energy resources in northern Europe: analyses using a regional climate 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super-high-resolution global and regional atmospheric models in the KAKUSHIN program"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206503248640","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Projections of Future Changes in Precipitation and the Vertical Structure of the Frontal Zone during the Baiu Season in the Vicinity of Japan Using a 5-km-mesh Regional Climate Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206503516672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Assessment of Ocean Surface Winds and Tropical Cyclones around Japan by RCMs"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206504116992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Development and Validation of a New Land Surface Model for JMA’s Operational Global Model Using the CEOP Observation 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Northeastern Japan in CMIP3 Multi-Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681479948288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Summertime Temperature Extremes over Japan in the Late 21st Century Projected by a High-Resolution Regional Climate Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681481226624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"ENSOイベント期間中の西部北太平洋表層水温場"},{"@language":"en","@value":"Surface Thermal Conditions in the Western North Pacific during the ENSO Events"}]},{"@id":"https://cir.nii.ac.jp/crid/1390579476808023040","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Assessment of extreme local topographic winds and their future changes from a massive high-resolution ensemble climate 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