{"_buckets": {"deposit": "18111e93-06bb-41eb-ab31-e4e477711cb6"}, "_deposit": {"id": "33681", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "33681"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00033681", "sets": []}, "author_link": ["131576", "131575"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "17. \u6ce2\u6e90\u57df\u306b\u304a\u3051\u308b\u6d25\u6ce2[II]"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1964-08-25", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "2", "bibliographicPageEnd": "381", "bibliographicPageStart": "369", "bibliographicVolumeNumber": "42", "bibliographic_titles": [{"bibliographic_title": "\u6771\u4eac\u5927\u5b78\u5730\u9707\u7814\u7a76\u6240\u5f59\u5831 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]}, "item_4_description_13": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_4_description_5": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "This work is the continuation of the previous study on the generation of a tsunami in the near field for a three-dimensional case, which has been done by means of numerical calculation resorting to an electronic computer. The method of analysis follows nearly the same line as that in the previous paper of the same title. Such a method, with a little modification, makes it possible to compute further the wave height of a tsunami in the near field, even though it is very low in efficiency. According to the results of the computation, it turns out that: (1) the variation of waves at the central part is more rapid than in other parts: (2) as far as the later phase is concerned, at the central part of the wave origin and only in this part, the motion of the waves goes above the mean level of water. In other words, in the parts excluding the center the undulations are superposed on the tail of the long wave. From the second reason described above, the approximation of the shallow water seems to be still in use for the analysis of the phenomena in the present stage (t*=21\uff5e45).", "subitem_description_type": "Abstract"}, {"subitem_description": "\u672c\u5831\u544a\u306f,\u6ce2\u6e90\u57df\u306b\u304a\u3051\u308b\u6d25\u6ce2\u3092\u96fb\u5b50\u8a08\u7b97\u6a5f\u3092\u7528\u3044\u3066\u89e3\u660e\u3057\u305f\u524d\u5831\u544a\u306e\u7d9a\u304d\u3067\u3042\u308a,\u524d\u5831\u544a\u3067\u306f,\u7b2c1\u6ce2\u306e\u5909\u5316\u3092\u4e3b\u306b\u8ad6\u3058\u305f\u306e\u306b\u5bfe\u3057,\u672c\u5831\u544a\u3067\u306f,\u7b2c2\u6ce2\u4ee5\u4e0b(later phase)\u306e\u6ce2\u306b\u3064\u3044\u3066,\u6570\u5024\u89e3\u6790\u3092\u304a\u3053\u306a\u3064\u305f.\u6570\u5024\u89e3\u6790\u306e\u65b9\u6cd5\u306f,\u524d\u5831\u544a\u3067\u7528\u3044\u305f\u306e\u3068\u307b\u307c\u540c\u3058\u3067,\u7a4d\u5206\u3059\u308b\u3068\u304d\u306e\u5206\u5272\u65b9\u6cd5\u3092\u5c11\u3057\u5909\u3048\u305f\u3060\u3051\u3067\u3042\u308b.\u8a08\u7b97\u7d50\u679c\u306b\u3088\u308c\u3070,(1)\u6ce2\u6e90\u57df\u306e\u4e01\u5ea6\u4e2d\u5fc3\u306b\u304a\u3051\u308b\u6d25\u6ce2\u306e\u5909\u5316\u306f\u4ed6\u306e\u90e8\u5206\u306e\u5909\u5316\u306b\u6bd4\u3079\u3066\u65e9\u304f\u9032\u884c\u3059\u308b.", "subitem_description_type": "Abstract"}]}, "item_4_full_name_3": {"attribute_name": "\u8457\u8005\u5225\u540d", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "131576", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "\u6311\u4e95, \u9ad8\u592b"}]}]}, "item_4_identifier_registration": {"attribute_name": "ID\u767b\u9332", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15083/0000033681", "subitem_identifier_reg_type": "JaLC"}]}, "item_4_publisher_20": {"attribute_name": "\u51fa\u7248\u8005", "attribute_value_mlt": [{"subitem_publisher": "\u6771\u4eac\u5927\u5b66\u5730\u9707\u7814\u7a76\u6240"}]}, "item_4_source_id_10": {"attribute_name": "\u66f8\u8a8c\u30ec\u30b3\u30fc\u30c9ID", "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": "\u65e5\u672c\u5341\u9032\u5206\u985e\u6cd5", "attribute_value_mlt": [{"subitem_subject": "453", "subitem_subject_scheme": "NDC"}]}, "item_4_text_21": {"attribute_name": "\u51fa\u7248\u8005\u5225\u540d", "attribute_value_mlt": [{"subitem_text_value": "Earthquake Research Institute, University of Tokyo"}]}, "item_4_text_34": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"subitem_text_value": "Departmental Bulletin Paper"}]}, "item_4_text_4": {"attribute_name": "\u8457\u8005\u6240\u5c5e", "attribute_value_mlt": [{"subitem_text_value": "Graduate School, the University of Tokyo"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "MOMOI, Takao"}], "nameIdentifiers": [{"nameIdentifier": "131575", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "\u30d5\u30a1\u30a4\u30eb\u60c5\u5831", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2017-06-26"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "ji0422003.pdf", "filesize": [{"value": "566.8 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 566800.0, "url": {"label": "ji0422003.pdf", "url": "https://repository.dl.itc.u-tokyo.ac.jp/record/33681/files/ji0422003.pdf"}, "version_id": "3490b3d6-4166-486d-99c8-133cc414e372"}]}, "item_language": {"attribute_name": "\u8a00\u8a9e", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_resource_type": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"resourcetype": "departmental bulletin paper", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "17. Tsunami in the Vicinity of a Wave Origin[II]", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "17. Tsunami in the Vicinity of a Wave Origin[II]", "subitem_title_language": "en"}]}, "item_type_id": "4", "owner": "1", "path": ["80/4535/4957/4963", "9/504/4538/4959/4964"], "permalink_uri": "https://doi.org/10.15083/0000033681", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2008-05-30"}, "publish_date": "2008-05-30", "publish_status": "0", "recid": "33681", "relation": {}, "relation_version_is_last": true, "title": ["17. Tsunami in the Vicinity of a Wave Origin[II]"], "weko_shared_id": -1}