{"created":"2023-06-19T12:43:31.114908+00:00","id":2878,"links":{},"metadata":{"_buckets":{"deposit":"260ff379-65d0-418f-8ce7-659a359364a4"},"_deposit":{"created_by":3,"id":"2878","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"2878"},"status":"published"},"_oai":{"id":"oai:tokyo-metro-u.repo.nii.ac.jp:00002878","sets":["521:522:524:525:548"]},"author_link":["7972","7973"],"item_3_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1990","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"25","bibliographicPageEnd":"268","bibliographicPageStart":"261","bibliographic_titles":[{"bibliographic_title":"Geographical Reports of Tokyo Metropolitan University"}]}]},"item_3_creator_2":{"attribute_name":"著者(ヨミ)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"スズキ, ケイスケ"}],"nameIdentifiers":[{"nameIdentifier":"7973","nameIdentifierScheme":"WEKO"}]}]},"item_3_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"This paper describes the effects of the drainage basin characteristics on the fluctuation of river runoff. The drainage basin characteristics influence the amount and rate of water yield and the shape of hydrograph. The drainage basin characteristics are controlled by topographic condition, rock and sediment type, vegetation and land use. Most variable characteristic of Icelandic rivers is the permeability of rock. Iceland is a part of the Mid-Atlantic Ridge and active volcanic zone, that is the highest permeable area, runs across the island. The Tertiary strata which are almost impermeable are exposed at the northwestern and eastern part of Iceland. Icelandic rivers are divided into three groups by the fluctuation pattern of runoff. \"Glacier river\": The amount of runoff varies annualy; very large in summer and very little in winter. \"Spring-fed river\": The amount of runoff is very even all the year round and is not affected by rainfall and snowmelt. This type river is mainly found in the highest permeable area of the central zone. \"Direct runoff river\": The fluctuation of runoff is very much dependent on the fluctuations of rainfall and snowmelt, and is very anomalous. This type river is found in the area of the impermeable basaltic rocks.","subitem_description_type":"Abstract"}]},"item_3_publisher_33":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"Department of Geography, Tokyo Metropolitan University"}]},"item_3_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA00200173","subitem_source_identifier_type":"NCID"}]},"item_3_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"03868710","subitem_source_identifier_type":"ISSN"}]},"item_3_version_type_16":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Suzuki, Keisuke"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-08-04"}],"displaytype":"detail","filename":"20005-25-022.pdf","filesize":[{"value":"430.4 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"20005-25-022.pdf","url":"https://tokyo-metro-u.repo.nii.ac.jp/record/2878/files/20005-25-022.pdf"},"version_id":"aa49cdf5-77e7-455a-8fc7-f531b5e8b500"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Iceland","subitem_subject_scheme":"Other"},{"subitem_subject":"fluctuation pattern of runoff","subitem_subject_scheme":"Other"},{"subitem_subject":"auto correlation coefficient","subitem_subject_scheme":"Other"},{"subitem_subject":"coefficient of variation","subitem_subject_scheme":"Other"},{"subitem_subject":"glacier river","subitem_subject_scheme":"Other"},{"subitem_subject":"spring-fed river","subitem_subject_scheme":"Other"},{"subitem_subject":"direct runoff river","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Classification of icelandic rivers by the fluctuation patterns of runoff","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Classification of icelandic rivers by the fluctuation patterns of runoff"}]},"item_type_id":"3","owner":"3","path":["548"],"pubdate":{"attribute_name":"公開日","attribute_value":"2010-11-30"},"publish_date":"2010-11-30","publish_status":"0","recid":"2878","relation_version_is_last":true,"title":["Classification of icelandic rivers by the fluctuation patterns of runoff"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-06-19T18:26:19.745946+00:00"}