{"created":"2021-03-01T06:14:40.072381+00:00","id":11769,"links":{},"metadata":{"_buckets":{"deposit":"f4c00255-9e06-4bf4-af34-0863bb5a39ba"},"_deposit":{"id":"11769","owners":[],"pid":{"revision_id":0,"type":"depid","value":"11769"},"status":"published"},"_oai":{"id":"oai:soar-ir.repo.nii.ac.jp:00011769","sets":["1169:1170"]},"author_link":["36067","36068","36069"],"item_1628147817048":{"attribute_name":"出版タイプ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_6_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2013","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"4","bibliographicPageEnd":"693","bibliographicPageStart":"682","bibliographicVolumeNumber":"122","bibliographic_titles":[{"bibliographic_title":"地学雑誌"}]}]},"item_6_description_20":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Observed discharge data covering the last three decades (1980-2009) at 16 rivers (i.e., rivers of Ida, Jinzu, Kurobe, Hime, Seki, Sai, Chikuma, Shinano, Uono, Kiso, Tenryu, Keta, Oi, Kamanashi, Fuefuki, and Fuji) in the Japanese Alps region are analyzed to clarify the elevation dependence of runoff characteristics during the snowmelt season. In the Hokuriku area, where large quantities of snow fall, the center time (CT) of snowmelt runoff tends to be delayed more at rivers with higher catchment-mean-elevations. In addition, the long-term (1980-2009) trend of a forward shift of snowmelt runoff timing becomes more remarkable at rivers in this area, with the exception of Hime River, as catchment-mean-elevation increases. However, the correlation between flowering dates of cherry trees and snowmelt runoff timing is stronger at rivers in the area with a lower catchment-mean-elevation. Consequently, snowmelt runoff at lower elevations in the Hokuriku area is sensitive to year-to-year fluctuations of spring onset, while progressive warming has greater impacts on snowmelt runoff timing at higher elevations, not only in winter to early spring but also in winter to late spring or summer. On the other hand, elevation dependence of snowmelt runoff timing is not detected at rivers in other areas; the runoff characteristics described above are neither clear nor statistically significant at both lower and higher elevations. Our results prove that the hydrological response to global warming is elevation dependent in a snow-dominated region, providing important knowledge for better water-resource management and flood control.","subitem_description_type":"Abstract"}]},"item_6_description_30":{"attribute_name":"資源タイプ(コンテンツの種類)","attribute_value_mlt":[{"subitem_description":"Article","subitem_description_type":"Other"}]},"item_6_description_5":{"attribute_name":"引用","attribute_value_mlt":[{"subitem_description":"地学雑誌. 122(4):682-693 (2013)","subitem_description_type":"Other"}]},"item_6_link_3":{"attribute_name":"信州大学研究者総覧へのリンク","attribute_value_mlt":[{"subitem_link_text":"鈴木, 啓助","subitem_link_url":"http://soar-rd.shinshu-u.ac.jp/profile/ja.upTmOUkh.html"}]},"item_6_publisher_4":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京地学協会"}]},"item_6_relation_48":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"10.5026/jgeography.122.682"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://doi.org/10.5026/jgeography.122.682","subitem_relation_type_select":"DOI"}}]},"item_6_source_id_35":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0022-135X","subitem_source_identifier_type":"ISSN"}]},"item_6_source_id_40":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00322536","subitem_source_identifier_type":"NCID"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"山中, 勤"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"脇山, 義史"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"鈴木, 啓助"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2015-09-28"}],"displaytype":"detail","filename":"Chigaku_Zasshi_122_4_682.pdf","filesize":[{"value":"1.3 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"Chigaku_Zasshi_122_4_682.pdf","url":"https://soar-ir.repo.nii.ac.jp/record/11769/files/Chigaku_Zasshi_122_4_682.pdf"},"version_id":"c9e16be0-5910-4445-95ce-917347146110"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"融雪流出","subitem_subject_scheme":"Other"},{"subitem_subject":"snowmelt runoff","subitem_subject_scheme":"Other"},{"subitem_subject":"河川流量","subitem_subject_scheme":"Other"},{"subitem_subject":"river discharge","subitem_subject_scheme":"Other"},{"subitem_subject":"気候変動","subitem_subject_scheme":"Other"},{"subitem_subject":"climatic change","subitem_subject_scheme":"Other"},{"subitem_subject":"中部山岳地域","subitem_subject_scheme":"Other"},{"subitem_subject":"Japanese Alps region","subitem_subject_scheme":"Other"},{"subitem_subject":"山岳水文","subitem_subject_scheme":"Other"},{"subitem_subject":"mountain hydrology","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"中部山岳地域における融雪流出特性の標高依存性","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"中部山岳地域における融雪流出特性の標高依存性","subitem_title_language":"ja"}]},"item_type_id":"6","owner":"1","path":["1170"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2013-10-04"},"publish_date":"2013-10-04","publish_status":"0","recid":"11769","relation_version_is_last":true,"title":["中部山岳地域における融雪流出特性の標高依存性"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-14T04:39:02.577776+00:00"}