{"_buckets": {"deposit": "98a645b1-898e-4b28-bf67-9e92b984072f"}, "_deposit": {"id": "32990", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "32990"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00032990", "sets": []}, "author_link": ["128622", "128621"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "\u6d77\u5e95\u659c\u9762\u306e\u6c34\u5e73\u306a\u52d5\u304d\u306b\u3088\u308a\u767a\u751f\u3059\u308b\u6d25\u6ce2\u306e\u5b9f\u9a13\u7684\u7814\u7a76"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1982-09-30", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "2", "bibliographicPageEnd": "262", "bibliographicPageStart": "239", "bibliographicVolumeNumber": "57", "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": "A tsunami generated by a transient horizontal motion of a sloping bottom is discussed experimentally. The experiment was performed in a channel by varying three independent parameters S, L and z, which represent the bottom slope near one end of the tank, the total horizontal displacement and the rise time of the bottom movement, respectively. About the maximum run-up of the water\u0027s edge, the following characteristics are found for moderate values of L and z. 1) For S=1/1, the run-up height exhibits analogous behavior to the wave generated by the horizontal motion of a vertical wall. 2) For S\u003c 1/3, the run-up height is dominated by a vertical component of the horizontal displacement, namely, LS. 3) Wave characteristics are well described by a linear-long wave theory. 4) Unified interpretation is possible for three different mechanisms of wave generation; the vertical motion of a horizontal bottom, the horizontal motion of a vertical wall, and the horizontal motion of a sloping bottom.", "subitem_description_type": "Abstract"}, {"subitem_description": "\u6d77\u5e95\u659c\u9762\u306e\u6c34\u5e73\u306a\u52d5\u304d\u306b\u3088\u308b\u6d25\u6ce2\u3092\u5b9f\u9a13\u7684\u306b\u8b70\u8ad6\u3057\u305f.\u5b9f\u9a13\u306f,\u5730\u9707\u7814\u7a76\u6240\u5730\u4e0b\u5b9f\u9a13\u6c34\u69fd\u3092\u7528\u3044,3\u3064\u306e\u72ec\u7acb\u306a\u30d1\u30e9\u30e1\u30fc\u30bf\u30fc,S,L,\u03c4\u3067\u3092\u5909\u5316\u3055\u305b\u3066\u884c\u306a\u3063\u305f.S\u306f\u50be\u659c\u58c1\u306e\u50be\u304d\u3067\u3042\u308a,L\u306f\u6c34\u5e73\u5909\u4f4d,\u03c4\u306f\u7acb\u3061\u4e0a\u304c\u308a\u6642\u9593\u3067\u3042\u308b.\u6700\u5927\u306f\u3044\u4e0a\u308a\u9ad8\u306b\u95a2\u3057\u3066,\u4ee5\u4e0b\u306e\u4e8b\u5b9f\u304c\u660e\u3089\u304b\u306b\u306a\u3063\u305f.1)S=1/1\u306e\u5834\u5408,\u6700\u5927\u306f\u3044\u4e0a\u304c\u308a\u9ad8\u306f,\u925b\u76f4\u58c1\u306e\u6c34\u5e73\u306a\u52d5\u304d\u306b\u3088\u308b\u3082\u306e\u3068,\u540c\u69d8\u306e\u50be\u5411\u3092\u793a\u3059.2)S\u003c1/3\u3067\u306f,\u6700\u5927\u306f\u3044\u4e0a\u304c\u308a\u9ad8\u306f,\u5909\u4f4d\u306e\u925b\u76f4\u6210\u5206LS\u306b\u652f\u914d\u3055\u308c\u308b.3)\u767a\u751f\u3057\u305f\u6ce2\u306e\u6027\u8cea\u306f,\u7dda\u578b\u9577\u6ce2\u7406\u8ad6\u3067\u3088\u304f\u8a18\u8ff0\u3055\u308c\u308b.4)3\u3064\u306e\u7570\u306a\u308b\u6ce2\u306e\u767a\u751f\u6a5f\u69cb,\u4e00\u69d8\u6c34\u6df1\u6d77\u5e95\u306e\u925b\u76f4\u5909\u4f4d\u30e2\u30c7\u30eb,\u925b\u76f4\u58c1\u306e\u6c34\u5e73\u5909\u4f4d\u30e2\u30c7\u30eb,\u50be\u659c\u58c1\u306e\u6c34\u5e73\u5909\u4f4d\u30e2\u30c7\u30eb\u306b\u95a2\u3057\u3066,\u7d71\u4e00\u7684\u306a\u89e3\u91c8\u304c\u53ef\u80fd\u3067\u3042\u308b.", "subitem_description_type": "Abstract"}]}, "item_4_full_name_3": {"attribute_name": "\u8457\u8005\u5225\u540d", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "128622", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "\u5ca9\u5d0e, \u4f38\u4e00"}]}]}, "item_4_identifier_registration": {"attribute_name": "ID\u767b\u9332", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15083/0000032990", "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": "\u5730\u9707\u7814\u7a76\u6240"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Iwasaki, Sin\u0027iti"}], "nameIdentifiers": [{"nameIdentifier": "128621", "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": "ji0572004.pdf", "filesize": [{"value": "1.3 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 1300000.0, "url": {"label": "ji0572004.pdf", "url": "https://repository.dl.itc.u-tokyo.ac.jp/record/32990/files/ji0572004.pdf"}, "version_id": "5b5e9317-dfe2-4fdd-a497-0cd414c62242"}]}, "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": "Experimental Study of a Tsunami Generated by a Horizontal Motion of a Sloping Bottom", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "Experimental Study of a Tsunami Generated by a Horizontal Motion of a Sloping Bottom", "subitem_title_language": "en"}]}, "item_type_id": "4", "owner": "1", "path": ["80/4535/4807/4813", "9/504/4538/4809/4814"], "permalink_uri": "https://doi.org/10.15083/0000032990", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2008-05-30"}, "publish_date": "2008-05-30", "publish_status": "0", "recid": "32990", "relation": {}, "relation_version_is_last": true, "title": ["Experimental Study of a Tsunami Generated by a Horizontal Motion of a Sloping Bottom"], "weko_shared_id": -1}