{"created":"2021-03-01T06:52:21.859272+00:00","id":33568,"links":{},"metadata":{"_buckets":{"deposit":"b0adb81c-221d-4ded-97a1-f702989001d1"},"_deposit":{"id":"33568","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"33568"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00033568","sets":["80:4535:4937:4943","9:504:4538:4939:4944"]},"author_link":["131153","131152"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"半円形の半島をおそった津波の回折 : 続報"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1966-10-31","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"480","bibliographicPageStart":"473","bibliographicVolumeNumber":"44","bibliographic_titles":[{"bibliographic_title":"東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]},"item_4_description_13":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_4_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"In this paper, further calculations of the waves around a peninsula were made. Then it is found that: (1) large wave height takes place near the root of a peninsula (which has already been ascertained in the previous paper), (2) rotating waves appear in a nearby part of the peninsula, (3) the incident waves are reflected in two parts, i.e., near the root of a peninsula and in a part of the tip of a headland and, between the above two zones of reflection, a discriminative line of discontinuity of phases is found.","subitem_description_type":"Abstract"},{"subitem_description":"前報告に続き本報告において,半島のまわりにおける津波の様子が論じられている.数値計算の結果,次のことが知られる. (1) 半島の根元近くに波高の大きい所が現われる(これはすでに前報告で知られている), (2) 沖合に回転する波が現われる, (3)進入波は2つの部分で反射される,すなわち半島の根元の近くと半島の先端近くとである.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"131153","nameIdentifierScheme":"WEKO"}],"names":[{"name":"桃井, 高夫"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000033568","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京大学地震研究所"}]},"item_4_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00162258","subitem_source_identifier_type":"NCID"}]},"item_4_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"00408972","subitem_source_identifier_type":"ISSN"}]},"item_4_subject_15":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"453","subitem_subject_scheme":"NDC"}]},"item_4_text_21":{"attribute_name":"出版者別名","attribute_value_mlt":[{"subitem_text_value":"Earthquake Research Institute, University of Tokyo"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Momoi, Takao"}],"nameIdentifiers":[{"nameIdentifier":"131152","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":"2017-06-26"}],"displaytype":"detail","filename":"ji0442002.pdf","filesize":[{"value":"278.4 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0442002.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/33568/files/ji0442002.pdf"},"version_id":"ae18367a-179e-4786-8966-f1946ff19363"}]},"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":"A Further Study of Diffraction of Tsunami Invading a Semi-circular Peninsula","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"A Further Study of Diffraction of Tsunami Invading a Semi-circular Peninsula","subitem_title_language":"en"}]},"item_type_id":"4","owner":"1","path":["4943","4944"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-05-30"},"publish_date":"2008-05-30","publish_status":"0","recid":"33568","relation_version_is_last":true,"title":["A Further Study of Diffraction of Tsunami Invading a Semi-circular Peninsula"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:08:53.562861+00:00"}