{"created":"2021-03-01T06:14:39.524220+00:00","id":11760,"links":{},"metadata":{"_buckets":{"deposit":"c0b81569-f6df-4602-819b-a593e7cdd9db"},"_deposit":{"id":"11760","owners":[],"pid":{"revision_id":0,"type":"depid","value":"11760"},"status":"published"},"_oai":{"id":"oai:soar-ir.repo.nii.ac.jp:00011760","sets":["1169:1170"]},"author_link":["36042","36043"],"control_number":"11760","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":"2010","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"26","bibliographicPageStart":"17","bibliographicVolumeNumber":"28","bibliographic_titles":[{"bibliographic_title":"Bulletin of Glaciological Research"}]}]},"item_6_description_20":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Spatial variability of the chemical constituents of winter precipitation on the eastern-western slopes of Mt. Norikura (alt. 3025m) of Japan Northern Alps was examined to clarify the transport process of aerosol that flows over the mountain barrier. The concentrations of chemical constituents in the snow recorded at the upper part of the mountain (above alt. 2420m) make a little difference. However, at the lower part of the mountain (below alt. 2420m), Cl- concentration in the snow on the eastern slope was lower than that on the western slope; non-sea-salt SO42- (nssSO42-), NO3-, nssCa2+, nssMg2+ and NH4+ concentrations on the eastern slope was higher than that on the western slope. The prevailing westerlies raged at the western and alpine parts of the mountain. On the eastern part of the mountain, the easterlies were predominant. We infer that the snow below an altitude of 2420m, in comparison to the other parts of mountain, is under relatively greater influence of the local emission of the chemical constituents.","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":"Bulletin of Glaciological Research. 28:17-26 (2010)","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":"SUZUKl, Keisuke","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":"Japanese Society of Snow and Ice"}]},"item_6_relation_48":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"10.5331/bgr.28.17"}],"subitem_relation_type":"isIdenticalTo","subitem_relation_type_id":{"subitem_relation_type_id_text":"https://doi.org/10.5331/bgr.28.17","subitem_relation_type_select":"DOI"}}]},"item_6_rights_62":{"attribute_name":"権利","attribute_value_mlt":[{"subitem_rights":"© 2010 Japanese Society of Snow and Ice"}]},"item_6_source_id_35":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1345-3807","subitem_source_identifier_type":"PISSN"}]},"item_6_source_id_40":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA11582242","subitem_source_identifier_type":"NCID"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"TANAKA,  Motoki","creatorNameLang":"en"},{"creatorName":"田中, 基樹","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"36042","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"SUZUKl,  Keisuke","creatorNameLang":"en"},{"creatorName":"鈴木, 啓助","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"36043","nameIdentifierScheme":"WEKO"}]}]},"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":"BGR28P17_2010_17-26_TANAKA_SUZUKI.pdf","filesize":[{"value":"1.6 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"BGR28P17_2010_17-26_TANAKA_SUZUKI.pdf","url":"https://soar-ir.repo.nii.ac.jp/record/11760/files/BGR28P17_2010_17-26_TANAKA_SUZUKI.pdf"},"version_id":"d09dc6fd-a992-4c5e-b1b7-5ec0ac97e739"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"an Northern Alps","subitem_subject_scheme":"Other"},{"subitem_subject":"北アルプス","subitem_subject_scheme":"Other"},{"subitem_subject":"winter precipitation","subitem_subject_scheme":"Other"},{"subitem_subject":"冬季降水","subitem_subject_scheme":"Other"},{"subitem_subject":"chemical constituents","subitem_subject_scheme":"Other"},{"subitem_subject":"化学成分","subitem_subject_scheme":"Other"},{"subitem_subject":"mountain barrier","subitem_subject_scheme":"Other"},{"subitem_subject":"山岳地形","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":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Winter precipitation chemistry at a high elevation site of Japan Northern Alps","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Winter precipitation chemistry at a high elevation site of Japan Northern Alps","subitem_title_language":"en"},{"subitem_title":"北アルプスにおける冬季降水中の化学成分濃度","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":"11760","relation_version_is_last":true,"title":["Winter precipitation chemistry at a high elevation site of Japan Northern Alps"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-14T04:11:46.008987+00:00"}