{"@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/1390282680198409088.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/sola.2008-012"}},{"identifier":{"@type":"URI","@value":"http://www.jstage.jst.go.jp/article/sola/4/0/4_0_45/_pdf"}},{"identifier":{"@type":"NAID","@value":"130004940889"}}],"dc:title":[{"@language":"en","@value":"Statistical Analyses of Snowfall Distribution in the Niigata Area and its Relationship to the Wind Distribution"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Analyses of precipitation amounts and surface winds observed at weather stations were conducted to investigate the effect of the topography on the snowfall distribution in Niigata. The topographic effect on the precipitation, particularly in the Niigata plain, has not been well discussed although Akiyama (1981a, 1981b) discussed the relationship between the snowfall distribution in Niigata and the synoptic scale condition. Using an empirical orthogonal function analysis, the winter precipitation distribution from 1988 to 2007 in Niigata was categorized as plain-type (P-type) and mountain-type (M-type). The P-type precipitation occurs under an upper trough over the Sea of Japan. The synoptic westerly wind, brought by the lower trough near the Japan Islands, and the deep convective mixed layer will be responsible for the precipitation in the plains of Niigata and Hokuriku. In addition, the Noto Peninsula and the mountain range to the east of the Hokuriku area seem to play an dynamical role in the precipitation in the Niigata plain. The M-type precipitation occurs under the upper trough over Japan. The synoptic scale condition brings northwesterly wind, which causes a topographic updraft at the mountain slope, resulting in precipitation dominated in the Niigata mountain range."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282680198409088","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000283593530"}],"foaf:name":[{"@language":"en","@value":"Iwamoto Katsushi"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Snow and Ice Research Center, National Research Institute for Earth Science and Disaster 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日本気象学会"}],"prism:publicationDate":"2008","prism:volume":"4","prism:startingPage":"45","prism:endingPage":"48"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://www.jstage.jst.go.jp/article/sola/4/0/4_0_45/_pdf"}],"availableAt":"2008","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360294643753266688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamic and thermodynamic contributions of ENSO to winter precipitation in Japan: frequency and precipitation of synoptic weather patterns"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848659042685312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mapping of Japanese areas susceptible to snow cover change"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707357373824","@type":"Article","resourceType":"学術雑誌論文(journal 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simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206504827392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Structure and Maintenance Process of Stationary Double Snowbands along the Coastal Region"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206505581184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"日本海沿岸地域の大雪の時•空間変動"},{"@language":"en","@value":"Time and Spatial Variations of Heavy Snowfalls in the Japan Sea Coastal Region"},{"@value":"Time and Spatial Variations of Heavy Snowfalls in the Japan Sea Coastal Region Part II. Large-scale situations for typical spatial distributions of heavy snowfalls classified by EOF"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206507437696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristics of Synoptic Conditions for Heavy Snowfall in Western to Northeastern Japan Analyzed by the 5-km Regional Climate Ensemble Experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680198542080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Analysis of Regional Difference in Altitude Dependence of Snow Depth Using High Resolve Numerical Experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681477534336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Doppler Radar Study on the Successive Development of Snowbands at a Convergence Line near the Coastal Region of Hokuriku District"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681479875968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The JRA-25 Reanalysis"},{"@value":"Special edition on the JRA-25 reanalysis"},{"@value":"The JRA-25"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681480751872","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"冬の季節風と陸風の間に作られたメソスケール降雪帯の構造についてのドップラーレーダー解析"},{"@language":"en","@value":"Doppler Radar Analysis of the Structure of Mesoscale Snow Bands Developed between the Winter Monsoon and the Land Breeze"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681482298368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"日本海沿岸地域の大雪の時•空間変動"},{"@language":"en","@value":"Time and Spatial Variations of Heavy Snowfalls in the Japan Sea Coastal Region"},{"@value":"Time and Spatial Variations of Heavy Snowfalls in the Japan Sea Coastal Region Part I. Principal Time and Space Variations of Precipitation Described by EOF"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681482399744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Numerical Simulation of the Quasi-Stationary Snowband Observed over the Southern Coastal Area of the Sea of Japan on 16 January 2001"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238075477504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Regional Snowfall Distributions in a Japan-Sea Side Area of Japan Associated with Jet Variability and Blocking"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238084145152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spatial Patterns of Winter Precipitation in the North-Central Region (Hokuriku District) of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387451549706368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Structures and environment of explosively developing extratropical cyclones in the northwestern Pacific region"},{"@value":"Structure and environment of explosively developing extratropical cyclones in the northwestern Pacific region"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417136235904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Synoptic meteorological conditions of gamma-ray glows in winter thunderstorms"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:0031445075"},{"@type":"CROSSREF","@value":"10.2151/sola.2008-012"},{"@type":"CIA","@value":"130004940889"},{"@type":"OPENAIRE","@value":"doi_dedup___::107d445c7ebee0ab3d52a4526fa4ad42"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2019-012_references_DOI_PmvLgtmYuYOCJadpkoW3zbxm0e7"},{"@type":"CROSSREF","@value":"10.2151/sola.2019-016_references_DOI_PmvLgtmYuYOCJadpkoW3zbxm0e7"},{"@type":"CROSSREF","@value":"10.1007/s00382-021-06052-9_references_DOI_PmvLgtmYuYOCJadpkoW3zbxm0e7"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00538-2_references_DOI_PmvLgtmYuYOCJadpkoW3zbxm0e7"},{"@type":"CROSSREF","@value":"10.1080/02626667.2013.839874_references_DOI_PmvLgtmYuYOCJadpkoW3zbxm0e7"},{"@type":"CROSSREF","@value":"10.2151/sola.2014-005_references_DOI_PmvLgtmYuYOCJadpkoW3zbxm0e7"},{"@type":"CROSSREF","@value":"10.1007/s00382-020-05419-8_references_DOI_PmvLgtmYuYOCJadpkoW3zbxm0e7"},{"@type":"CROSSREF","@value":"10.1029/2022jd036996_references_DOI_PmvLgtmYuYOCJadpkoW3zbxm0e7"},{"@type":"CROSSREF","@value":"10.1007/s00382-020-05163-z_references_DOI_PmvLgtmYuYOCJadpkoW3zbxm0e7"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2018-022_references_DOI_PmvLgtmYuYOCJadpkoW3zbxm0e7"}]}