{"@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/1390282681479948288.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/jmsj.2012-a05"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"023526844"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/023526844"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I023526844"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/jmsj/90A/0/90A_2012-A05/_pdf"}},{"identifier":{"@type":"NAID","@value":"130004435183"}},{"identifier":{"@type":"NAID","@value":"40019200938"}}],"dc:title":[{"@language":"en","@value":"Summertime Temperature Extremes over Japan in the Late 21st Century Projected by a High-Resolution Regional Climate Model"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Future changes in summertime temperature extremes over Japan are projected by a well-developed regional climate model (RCM) with a spatial resolution of 5 km. The performance of the RCM with respect to temperature in the present climate is evaluated first based on observations. Although the differences in the biases (from observations) of daily temperatures between the RCM and the driving atmospheric general circulation model (AGCM) simulations are not statistically significant, root-mean-square errors (from observations) in daily mean and minimum temperatures reproduced by the RCM are smaller than those by the AGCM with a coarser spatial resolution. These results indicate that RCM with a higher spatial resolution has better performance than the driving AGCM in simulating temperature variability. A test of whether the RCM can capture temperature extremes reveals a good quantitative agreement between simulated and observed values in appearance frequency of extreme high temperature for the daily minimum temperature during July and August. The spatial pattern of the upper tail of the frequency distribution for the daily maximum temperature is also in good agreement with observations, although the model values are underestimated.<br>Projected changes for extremely high daily minimum temperature are relatively large in July on the lee side of the Hidaka Mountains, southeast of Hokkaido. This finding can be explained by the foehn phenomenon: changes in the windward Froude number indicate that atmospheric conditions in the future climate are more favorable for the intensification of foehn. In terms of extremely high daily maximum temperature, the difference between the present-day and future climates during August is relatively large over the Tama area, west of Tokyo. Although the foehn phenomenon is not solely responsible for the projected changes, the phenomenon can explain the projected changes when westerly winds prevail over the Tama area, located on the lee side of the Kanto Mountains."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@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 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Ser. II"},{"@language":"ja","@value":"気象集誌"},{"@language":"ja","@value":"氣象集誌. 第2輯"},{"@language":"en","@value":"Journal of the Meteorological Society of Japan"},{"@language":"en","@value":"JMSJ"}],"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":"2012","prism:volume":"90A","prism:number":"0","prism:startingPage":"101","prism:endingPage":"122"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/023526844"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I023526844"},{"@id":"https://www.jstage.jst.go.jp/article/jmsj/90A/0/90A_2012-A05/_pdf"}],"availableAt":"2012","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011145256055424","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Flux Parameterization over Land Surfaces for Atmospheric 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regional climate model in MRI"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680199989376","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Projection of Changes in Future Surface Wind around Japan Using a Non-hydrostatic Regional Climate Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681478332416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Foehn Event Enhanced by the Synoptic Scale Dry Intrusion"},{"@language":"ja-Kana","@value":"Foehn Event Enhanced by the Synoptic Scale Dry Intrusion"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681480705792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"夏の相模湾沿岸における海陸風の構造"},{"@language":"en","@value":"A Detailed Analysis of the Land and Sea Breeze in the Sagami Bay Area in Summer"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681480967680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"20-km-Mesh Global Climate Simulations Using JMA-GSM Model<br>—Mean Climate States—"},{"@value":"20-km-Mesh Global Climate Simulations Using JMA-GSM Model--Mean Climate States"},{"@value":"20-km-Mesh Global Climate Simulations Using JMA-GSM Model<br>&mdash;Mean Climate States&mdash;"},{"@value":"20-km-mesh global climate simulations using JMA-GSM model—Mean climate states"},{"@value":"20 km-mesh global climate simulations using JMA-GSM model—Mean climate state"},{"@value":"20-km-mesh global climate simulations using JMA-GSM model—mean climate states—"},{"@value":"20-km-Mesh global climate simulations using JMA-GSM Model<br>—Mean climate States&mdash;"},{"@value":"20km-Mesh global climate simulations using JMA-GSM model"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681481989248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Role of Large-Scale Circulation in Triggering Foehns in the Hokuriku District of Japan during Midsummer"},{"@value":"Role of large-scale circulation in triggering foehn in the Hokuriku district of Japan during midsummer"}]},{"@id":"https://cir.nii.ac.jp/crid/1390848250135056000","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Extreme Rainfall Projections for Malaysia at the End of 21st Century Using the High Resolution Non-Hydrostatic Regional Climate Model (NHRCM)"}]},{"@id":"https://cir.nii.ac.jp/crid/1520290883847793792","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"「21世紀気候変動予測革新プログラム」における,CMIP5実験仕様に基づいた温暖化予測実験"},{"@language":"ja-Kana","@value":"「 21セイキ キコウ ヘンドウ ヨソク カクシン プログラム 」 ニ オケル,CMIP5 ジッケン シヨウ ニ モトズイタ オンダンカ ヨソク 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