{"created":"2021-03-01T06:57:13.958560+00:00","id":37937,"links":{},"metadata":{"_buckets":{"deposit":"feb1616a-baa3-476c-838e-db7725d4a3a2"},"_deposit":{"id":"37937","owners":[],"pid":{"revision_id":0,"type":"depid","value":"37937"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00037937","sets":["75:5892:5950","9:504:5894:5951"]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1902-08-02","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"18","bibliographicPageStart":"1","bibliographicVolumeNumber":"16","bibliographic_titles":[{"bibliographic_title":"The journal of the College of Science, Imperial University of Tokyo, Japan = 東京帝國大學紀要. 理科"}]}]},"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":"A summary of the principal conclusions obtained from the above considerations is added here. A. The negative potential observed during strong wind is entirely due to the negative electrification of the dust raised and carried in the atmosphere, by friction with terrestrial objects. 2. Similarly the high potential observed during fog or haze is due to the positive electrification of the water particles composing it. 3. When a mass of cold air comes in contact with a mass of warm air, the former becomes positively electrified with respect to the latter. This fact is probably one of the causes which determine the normal distribution of the electric field in the atmosphere. Also it may account for the fact that an abnormally high potential is generally accompanied by an abnormally low temperature. 4. The invariably high potentials at or near sunrise are probably due to the fact that the air lying near the surface has then a temperature lower than that of the air above it, and becomes, in consequence positively electrified. 5. When two masses of air at different temperatures happen to be mixed suddenly, the electric field is violently disturbed. The disturbances are, however, just such as are in accord with the fact stated in 3. In conclusion, I wish to express my great indebtedness to Dr. K. Nakamura, director of the Central Meteorological Observatory, by whose kind permission, I have been able to examine several original records preserved in that observatory. The copies of photographs are also reproduced here through the courtesy of that gentleman. My best thanks are due to Professor Tanakadate and to Professor Nagaoka of the Tokyo University, who were kind enough to give me valuable suggestions, and to favour me with access to the literature of the subject.","subitem_description_type":"Abstract"}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/00037928","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"College of Science, Imperial University"}]},"item_4_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA00695779","subitem_source_identifier_type":"NCID"}]},"item_4_subject_15":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"427.53","subitem_subject_scheme":"NDC"}]},"item_4_text_21":{"attribute_name":"出版者別名","attribute_value_mlt":[{"subitem_text_value":"東京帝國大學理學部"}]},"item_4_text_4":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"Physics in First High School"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"HOMMA, Y."}],"nameIdentifiers":[{"nameIdentifier":"136784","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":"2017-06-27"}],"displaytype":"detail","filename":"jcs016007.pdf","filesize":[{"value":"1.1 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"jcs016007.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/37937/files/jcs016007.pdf"},"version_id":"b960a383-7ee0-4a81-91fc-1fdc825b07d9"}]},"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":"Studies in Atmospheric Electricity","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Studies in Atmospheric Electricity"}]},"item_type_id":"4","owner":"1","path":["5950","5951"],"pubdate":{"attribute_name":"公開日","attribute_value":"2010-02-03"},"publish_date":"2010-02-03","publish_status":"0","recid":"37937","relation_version_is_last":true,"title":["Studies in Atmospheric Electricity"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2022-12-19T04:12:33.274344+00:00"}