{"_buckets": {"deposit": "2fc3a365-c5a8-4e7a-a631-e737ae39e625"}, "_deposit": {"id": "33464", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "33464"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00033464", "sets": []}, "author_link": ["130707", "130706"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "6.\u9632\u6ce2\u5824\u306e\u307e\u308f\u308a\u306b\u304a\u3051\u308b\u9577\u6ce2 : \u5782\u76f4\u5165\u5c04\u306e\u5834\u5408[3\uff3d"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1968-03-19", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "1", "bibliographicPageEnd": "135", "bibliographicPageStart": "124", "bibliographicVolumeNumber": "46", "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": "In the present work, the calculations are carried out for the waves of large wave-length in the windward waters around the gap of the breakwater in order to examine the nature of the trapezoid of the crest lines, which was ascertained for the case of the long wave around an estuary in the previous work. The result of the computation reveals that the feature of the trapezoid appears in front of the gap of the breakwater in a form a little different from the trapezoid for the case of the long wave around the estuary and that the waves advancing to the entrance in the nearby waters of the terminus of the breakwater are retarded as the result of the collision of the waves with the breakwater wing. In the last part of this study, a brief note on the generation of the high waves along the windward part of the breakwater is made referring to other authors\u0027works, which show the appearance of the high waves near the terminus of the 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