{"@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/1390282681482246784.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/jmsj1965.59.1_26"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/jmsj1965/59/1/59_1_26/_pdf"}},{"identifier":{"@type":"NAID","@value":"130007346534"}}],"dc:title":[{"@language":"ja","@value":"0°C高度下の未飽和大気中で起こる雪片の非融解現象"},{"@language":"en","@value":"Non-Melting Phenomena of Snowflakes Observed in Subsaturated Air below Freezing Level"}],"description":[{"type":"abstract","notation":[{"@language":"en","@value":"The analyses of the meteorological surface data at Wajima, Matsumoto, and Nikko Weather Stations in Japan were made in order to examine the effect of relative humidity of air on melting of snowflakes below freezing level in the atmosphere. The results showed that the types of precipitations (rain or snow) observed on the ground were closely dependent on surface relative humidity as well as surface air temperature. When surface relative humidity was below a certain critical humidity, even at a higher surface air tempera- ture above 0°C precipitations were snow. Using the regression analysis, the relations of the critical relative humidity RHcri to surface air temperature T could be obtained at each Weather Station in the following forms, RHcri=-7.5<i>T</i>+93, ............... Wajima, RHcri=-7.3<i>T</i>+96, ............... Mtsumoto, RHcri=-6.2<i>T</i>+91, ............... Nikko.<br>The relations thus obtained agreed well with that obtained previously from the theoretical calculations by Matsuo and Sasyo (1981)."},{"@language":"ja","@value":"輪島,松本,日光測候所の地上気象観測データを使用して,雪片の融解に与える湿度の影響を解析的に調べた。地上で観測される降水のタイプ(雨,雪)は,地上気温のみならず湿度に依存して変化することが明らかになった。降雪は地上気温が0°C以上のかなり高い場合にも見られ,これは低い地上の湿度と関連していた。これらの降雪は,地上の湿度がある臨界値以下であれば必ず見られた。三地点の臨界湿度と地上気温の関係を回帰分析により求めると次のようになった。RHcri=-7.5<i>T</i>+93,輪島 RHcri=-7.3<i>T</i>+96,松本 RHcri=-6.2<i>T</i>+91,日光<br>得られた関係は松尾,佐粧(1981)が計算によって求めた雪片の融解開始時の温•湿度の関係式と良く一致した。"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282681482246784","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000392818037"}],"foaf:name":[{"@language":"ja","@value":"松尾 敬世"},{"@language":"en","@value":"Matsuo Takayo"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"},{"@language":"ja","@value":"気象研究所"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681482246785","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000392818038"}],"foaf:name":[{"@language":"ja","@value":"佐粧 純男"},{"@language":"en","@value":"Sasyo Yoshio"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"},{"@language":"ja","@value":"気象研究所"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00261165"},{"@type":"LISSN","@value":"00261165"},{"@type":"EISSN","@value":"21869057"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00261165"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/00261165"}],"prism:publicationName":[{"@language":"ja","@value":"気象集誌. 第2輯"},{"@value":"気象集誌. 第2輯"},{"@language":"en","@value":"Journal of the Meteorological Society of Japan. 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":"1981","prism:volume":"59","prism:number":"1","prism:startingPage":"26","prism:endingPage":"32"},"reviewed":"false","url":[{"@id":"https://www.jstage.jst.go.jp/article/jmsj1965/59/1/59_1_26/_pdf"}],"availableAt":"1981","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360026060099171968","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The JapanFlux2024 dataset for eddy covariance observations covering Japan and East Asia from 1990 to 2023"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568467813204736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Response of snowpack to +2°C global warming in Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206459331840","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Melting of snow pellets in the atmosphere."},{"@language":"ja","@value":"大気中における雪あられの融解について"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206503990016","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"二波長レーダーで観測される融解中の雪片の微物理過程"},{"@language":"en","@value":"Microphysical Processes of Melting Snowflakes Detected by Two-wavelength Radar"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206505543168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"0°C高度下における雪片の融解について"},{"@language":"en","@value":"Melting of Snowflakes below Freezing Level in the Atmosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206506822144","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地上で観測される降水の型と地上気象要素との関係"},{"@language":"en","@value":"Relationship between Types of Precipitation on the Ground and Surface Meteorological Elements"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681477384576","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"On the Near-0.DEG.C. Frequency Maximum in Surface Air Temperature under Precipitation: A Statistical Evidence for the Melting Effect."}]},{"@id":"https://cir.nii.ac.jp/crid/1390576745205310720","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spatio-temporal changes in precipitation type and its relationships with snow damages during the heavy snowfall event in the Kanto-Koshin district, February 2014"},{"@language":"ja","@value":"2014年2 月14-15日の関東甲信地方の大雪における降水形態と雪氷災害の地域性との関連"}]},{"@id":"https://cir.nii.ac.jp/crid/1390861305859666432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimation of Spatial Snowpack Properties in a Snow-Avalanche Release Area: An Extreme Case on Mt. 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