{"@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/1361699995043083392.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2307/1552623"}},{"identifier":{"@type":"DOI","@value":"10.1080/15230430.1999.12003281"}},{"identifier":{"@type":"URI","@value":"https://www.tandfonline.com/doi/pdf/10.1080/15230430.1999.12003281"}},{"identifier":{"@type":"NAID","@value":"30021535842"}}],"dc:title":[{"@value":"Hydrodynamics of a Supraglacial Lake and Its Effect on the Basin Expansion: Tsho Rolpa, Rolwaling Valley, Nepal Himalaya"}],"description":[{"notation":[{"@value":"The thermal structure and hydrodynamics of supraglacial Tsho Rolpa Lake (27?51'N, 86?29'E) in the Nepal Himalaya were examined in the premonsoon of 1996. We continuously measured flow velocity, water temperature, and turbidity with moored self-recording current meters, temperature data loggers, and turbidimeters. Vertical measurements (every 0.2 m in depth) of water temperature and turbidity were also made by lowering a self-recording sonde. Tsho Rolpa Lake (surface area, 1.39 km2 at present) has increased in size since late 1950s (surface area, 0.23 km2 in 1958) by both glacial ice melt below the lake bottom and the retreat of the glacier terminus. Lake stratification is defined by suspended sediment concentration (SSC) rather than by temperature. The suspended sediment is mostly silt and clay (d  -5?C) into continual contact with the glacier terminus. This warm water contact could induce calving of the upper glacier-ice by increasingly melting the subaqueous lower part."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699995043083392","@type":"Researcher","foaf:name":[{"@value":"Kazuhisa Chikita"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995043083394","@type":"Researcher","foaf:name":[{"@value":"Jageshwar Jha"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995043083393","@type":"Researcher","foaf:name":[{"@value":"Tomomi Yamada"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"15230430"},{"@type":"EISSN","@value":"19384246"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/15230430"}],"prism:publicationName":[{"@value":"Arctic, Antarctic, and Alpine Research"}],"dc:publisher":[{"@value":"Informa UK Limited"}],"prism:publicationDate":"1999-02","prism:volume":"31","prism:number":"1","prism:startingPage":"58"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"https://www.tandfonline.com/doi/pdf/10.1080/15230430.1999.12003281"}],"createdAt":"2006-04-18","modifiedAt":"2020-06-08","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002214350961664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermal structure of proglacial lakes in Patagonia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233291702272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nocturnal Thermal Fracturing of a Himalayan Debris‐Covered Glacier Revealed by Ambient Seismic Noise"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643802712832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Subglacial discharge controls seasonal variations in the thermal structure of a glacial lake in Patagonia"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204423258368","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"モレーン堰止型氷河湖の熱循環に与える地形の影響"},{"@language":"en","@value":"The effect of surrounding topography on the thermal water circulation in moraine-dammed glacial lakes:"},{"@value":"モレーン堰止型氷河湖の熱循環に与える地形の影響--ヒマラヤのイムジャ湖とツォー・ロルパ湖との比較"},{"@language":"ja-Kana","@value":"モレーン セキトメガタ ヒョウガコ ノ ネツ ジュンカン ニ アタエル チケイ ノ エイキョウ ヒマラヤ ノ イムジャコ ト ツォー ロルパコ トノ ヒカク"},{"@value":"The effect of surrounding topography on the thermal water circulation in moraine-dammed glacial lakes: Imja and Tsho Rolpa Lakes in the Himalayas"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681437090560","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Meteorological-hydrological environment and thermal regime of a moraine-dammed glacier lake, and their contribution to the lake expansion."},{"@value":"モレーン堰き止め氷河湖の拡大と気象・水文・熱環境"},{"@language":"ja-Kana","@value":"モレーン セキトメ ヒョウガコ ノ カクダイ ト キショウ スイモン ネツ カンキョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681437265536","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The expansion mechanism of moraine-dammed glacial lakes in the Himalayas from a hydrodynamic viewpoint"},{"@value":"ヒマラヤにおけるモレーン堰止型氷河湖の拡大機構について―湖水流動系の観点から―"},{"@language":"ja-Kana","@value":"ヒマラヤ ニ オケル モレーン セキトメガタ ヒョウガコ ノ カクダイ キコウ ニ ツイテ コ スイリュウドウケイ ノ カンテン カラ"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009750245147648","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"ネパールヒマラヤ、ロールワリン・ヒマールのツォー・ロルパ氷河湖における熱的環境"},{"@language":"en","@value":"Thermal regime of a moraine-dammed glacial lake, Tsho Rolpa, in Rolwaling Himal, Nepal Himalayas"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950399661853184","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"ブータン・ヒマラヤ、ルナナ地方における2002年氷河、氷河湖調査活動の概要"},{"@language":"en","@value":"Outline of 2002 - research activities on glaciers and glacier lakes in Lunana region, Bhutan Himalayas"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.2307/1552623"},{"@type":"CROSSREF","@value":"10.1080/15230430.1999.12003281"},{"@type":"CIA","@value":"30021535842"},{"@type":"OPENAIRE","@value":"doi_dedup___::413b3c3dd1487b13a4cd28cb31c4de4f"},{"@type":"CROSSREF","@value":"10.1002/2016jf004084_references_DOI_JklOvvv8gwrBtfFuXryyOEhr4hA"},{"@type":"CROSSREF","@value":"10.4145/jahs.37.93_references_DOI_EDEjcJvW4dpgI5GmK4tS7mxfTTV"},{"@type":"CROSSREF","@value":"10.1038/s41467-021-26578-0_references_DOI_EDEjcJvW4dpgI5GmK4tS7mxfTTV"},{"@type":"CROSSREF","@value":"10.1029/2018gl079653_references_DOI_JklOvvv8gwrBtfFuXryyOEhr4hA"}]}