{"created":"2021-03-01T06:25:54.726216+00:00","id":18497,"links":{},"metadata":{"_buckets":{"deposit":"2f2cc0c8-85f3-4c79-ad84-f34736fa1327"},"_deposit":{"id":"18497","owners":[],"pid":{"revision_id":0,"type":"depid","value":"18497"},"status":"published"},"_oai":{"id":"oai:nagoya.repo.nii.ac.jp:00018497"},"item_9_biblio_info_6":{"attribute_name":"\u66f8\u8a8c\u60c5\u5831","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1989-11","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"90","bibliographicPageStart":"83","bibliographicVolumeNumber":"36","bibliographic_titles":[{"bibliographic_title":"Proceedings of the Research Institute of Atmospherics, Nagoya University"}]}]},"item_9_description_4":{"attribute_name":"\u6284\u9332","attribute_value_mlt":[{"subitem_description":"The longitudinally asymmetric geomagnetic disturbances during the February 1986 storm are using the data from 10 middle latitude stations. Both H and D components are used to derive the asymmetry indices. The amplitude of the asymmetry in H and D is found to be on the same order of magnitude indicating that the field-aligned currents mainly contribute to the mid-latitude asymmetric disturbances rather than the partial ring current. The temporal variation of the asymmetry indices suggests a drastic switching of the large scale magnetospheric current system during the storm after the IMF northward turning.","subitem_description_type":"Abstract"}]},"item_9_description_5":{"attribute_name":"\u5185\u5bb9\u8a18\u8ff0","attribute_value_mlt":[{"subitem_description":"This special issue contains contributed papers presented at the symposium \"Solar Terrestrial Events in February-March 1986\" (January 19, 1989, Nagoya)","subitem_description_type":"Other"}]},"item_9_identifier_60":{"attribute_name":"URI","attribute_value_mlt":[{"subitem_identifier_type":"HDL","subitem_identifier_uri":"http://hdl.handle.net/2237/22048"}]},"item_9_publisher_32":{"attribute_name":"\u51fa\u7248\u8005","attribute_value_mlt":[{"subitem_publisher":"The Research Institute of Atmospherics, Nagoya University"}]},"item_9_select_15":{"attribute_name":"\u8457\u8005\u7248\u30d5\u30e9\u30b0","attribute_value_mlt":[{"subitem_select_item":"publisher"}]},"item_9_source_id_7":{"attribute_name":"ISSN\uff08print\uff09","attribute_value_mlt":[{"subitem_source_identifier":"0077-264X","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"\u8457\u8005","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Iyemori, T."}],"nameIdentifiers":[{"nameIdentifier":"53749","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Takahashi, S."}],"nameIdentifiers":[{"nameIdentifier":"53750","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":"2018-02-21"}],"displaytype":"detail","filename":"proria_36_2_83.pdf","filesize":[{"value":"562.3 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"proria_36_2_83.pdf","url":"https://nagoya.repo.nii.ac.jp/record/18497/files/proria_36_2_83.pdf"},"version_id":"450dbd0d-023b-4d85-8dd3-10afe89b3ea5"}]},"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":"DEVELOPMENT OF ASYMMETRIC MAGNETIC DISTURBANCE FIELDS IN MIDDLE LATITUDES DURING FEBRUARY 1986 STORM","item_titles":{"attribute_name":"\u30bf\u30a4\u30c8\u30eb","attribute_value_mlt":[{"subitem_title":"DEVELOPMENT OF ASYMMETRIC MAGNETIC DISTURBANCE FIELDS IN MIDDLE LATITUDES DURING FEBRUARY 1986 STORM"}]},"item_type_id":"9","owner":"1","path":["879/1183/1640/1641"],"pubdate":{"attribute_name":"\u516c\u958b\u65e5","attribute_value":"2015-05-27"},"publish_date":"2015-05-27","publish_status":"0","recid":"18497","relation_version_is_last":true,"title":["DEVELOPMENT OF ASYMMETRIC MAGNETIC DISTURBANCE FIELDS IN MIDDLE LATITUDES DURING FEBRUARY 1986 STORM"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2021-03-01T16:39:15.801473+00:00"}