{"created":"2023-07-25T11:01:44.113465+00:00","id":3840,"links":{},"metadata":{"_buckets":{"deposit":"e9a849dd-e767-4030-8b3d-51d6cda2509c"},"_deposit":{"created_by":4,"id":"3840","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"3840"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00003840","sets":["1259:1260:1262:524:532"]},"author_link":["6258","6260","6261","6259"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"FORMATION OF SIDE BRANCHES OF DENDRITIC ICE CRYSTALS GROWING FROM THE VAPOR PHASE"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1994-11","bibliographicIssueDateType":"Issued"},"bibliographicPageStart":"183","bibliographicVolumeNumber":"8","bibliographic_titles":[{"bibliographic_title":"Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology"}]}]},"item_1_creator_7":{"attribute_name":"著者名よみ","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"ゴンダ, タケヒコ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ワダ, マコト"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"GONDA, Takehiko","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"WADA, Makoto","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_1_description_1":{"attribute_name":"ページ属性","attribute_value_mlt":[{"subitem_description":"P(論文)","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"σ^* is the critical supersaturation where kinetic roughening takes place. When the supersaturation σ<γ^*, prismatic facets are formed at the tips of primary branches of dendritic ice crystal. Then, the side branches are formed as a result of the shape instability of the prismatic facets with changing supersaturation. In the next place, when the supersaturation σ>σ^*, the tip shape of primary branches of dendritic ice crystal becomes round. In this case, the side branches are formed as a result of the change in the tip width of primary branches with changing supersaturation. Snow crystals observed in Antarctica are discussed on the basis of these experimental results.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00003840","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"National Institute of Polar Research"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA10756213","subitem_source_identifier_type":"NCID"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Division of General Education, Aichi-Gakuin University"},{"subitem_text_language":"en","subitem_text_value":"National Institute of Polar Research"}]},"item_1_text_3":{"attribute_name":"記事種別(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"ABSTRACT"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1994-11-01"}],"displaytype":"detail","filename":"KJ00000767948.pdf","filesize":[{"value":"56.1 kB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000767948","url":"https://nipr.repo.nii.ac.jp/record/3840/files/KJ00000767948.pdf"},"version_id":"20d18ae8-7099-4122-bb14-56155d713e43"}]},"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":"FORMATION OF SIDE BRANCHES OF DENDRITIC ICE CRYSTALS GROWING FROM THE VAPOR PHASE","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"FORMATION OF SIDE BRANCHES OF DENDRITIC ICE CRYSTALS GROWING FROM THE VAPOR PHASE"}]},"item_type_id":"1","owner":"4","path":["532"],"pubdate":{"attribute_name":"公開日","attribute_value":"1994-11-01"},"publish_date":"1994-11-01","publish_status":"0","recid":"3840","relation_version_is_last":true,"title":["FORMATION OF SIDE BRANCHES OF DENDRITIC ICE CRYSTALS GROWING FROM THE VAPOR PHASE"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:28:00.377723+00:00"}