{"created":"2023-06-20T15:05:56.189917+00:00","id":35305,"links":{},"metadata":{"_buckets":{"deposit":"06ec50e6-86b9-4a73-a173-31dc301a8c22"},"_deposit":{"created_by":1,"id":"35305","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"35305"},"status":"published"},"_oai":{"id":"oai:jaxa.repo.nii.ac.jp:00035305","sets":["1887:1890","1896:1898:1899:1993"]},"author_link":["421606","421603","421605","421601","421602","421604"],"item_9_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"對流の理論的及び實驗的研究と其の海陸風への應用"}]},"item_9_biblio_info_10":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1937-02","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"145","bibliographicPageEnd":"67","bibliographicPageStart":"1","bibliographicVolumeNumber":"12","bibliographic_titles":[{"bibliographic_title":"東京帝國大學航空研究所報告"},{"bibliographic_title":"Report of Aeronautical Research Institute, Tokyo Imperial University","bibliographic_titleLang":"en"}]}]},"item_9_description_17":{"attribute_name":"抄録（英）","attribute_value_mlt":[{"subitem_description":"The motion of the fluid developed when one half of its bottom was heated was solved mathematically, and the solution was compared with schematic experiments and also with observed data of sea breezes. The schematic experiments were carried out with water in a tank. A vertical temperature gradient, which corresponds to the gradient of the potential temperature in the atmosphere, was given to the water. And then, the temperature of one half of the bottom of the tank was raised a few degrees. In this way, a circulation of elliptic paths was generated above the boundary of the warm and the cold halves. The velocities of the water and the speed of growth of the circulation were measured. The mathematical solution accords well with the results of the experiments, if a suitable value is given to the diffusibility of temperature in a verical direction, which the solution contains, and the effect of visccsity is taken into consideration. In the case of sea breeze, the mathematical solution gives the relations of the rate of rising of the temperature on the earth's surface by the solar radiation to the wind velocities at various points and times, the height of the limit of the breeze and the speed of extension inland of the region covered by the breeze.","subitem_description_type":"Other"}]},"item_9_description_32":{"attribute_name":"資料番号","attribute_value_mlt":[{"subitem_description":"資料番号: SA4146474000","subitem_description_type":"Other"}]},"item_9_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京帝國大學航空研究所"}]},"item_9_publisher_9":{"attribute_name":"出版者（英）","attribute_value_mlt":[{"subitem_publisher":"Aeronautical Research Institute, Tokyo Imperial University"}]},"item_9_source_id_24":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA00387631","subitem_source_identifier_type":"NCID"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"小林, 辰男"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"佐々木, 達治郎"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"長内, 忠雄"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"KOBAYASI, Tatuo","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"SASAKI, Tatudiro","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"OSANAI, Tadao","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2020-01-24"}],"displaytype":"detail","filename":"SA4146474.pdf","filesize":[{"value":"2.6 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"SA4146474.pdf","url":"https://jaxa.repo.nii.ac.jp/record/35305/files/SA4146474.pdf"},"version_id":"0264c5c3-a2dc-4753-9ef7-61d304990535"}]},"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":"Theoretical and Experimental Studies of Convectional Circulation and its Relation to Land and Sea-breezes","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Theoretical and Experimental Studies of Convectional Circulation and its Relation to Land and Sea-breezes","subitem_title_language":"en"}]},"item_type_id":"9","owner":"1","path":["1890","1993"],"pubdate":{"attribute_name":"公開日","attribute_value":"2015-03-26"},"publish_date":"2015-03-26","publish_status":"0","recid":"35305","relation_version_is_last":true,"title":["Theoretical and Experimental Studies of Convectional Circulation and its Relation to Land and Sea-breezes"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-06-20T23:22:19.984956+00:00"}