{"created":"2023-07-25T11:00:55.510314+00:00","id":2841,"links":{},"metadata":{"_buckets":{"deposit":"1537fc92-49ce-456f-981c-3cfe65472eb9"},"_deposit":{"created_by":4,"id":"2841","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"2841"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00002841","sets":["1259:1260:1265:414:424"]},"author_link":["3550","3553","3551","3552"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"APPLICABILITY OF 10Hz SATELLITE ALTIMETRY DATA TO THE ANTARCTIC MARGIN"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1997-09","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"35","bibliographicPageStart":"26","bibliographicVolumeNumber":"10","bibliographic_titles":[{"bibliographic_title":"Proceedings of the NIPR Symposium on Antarctic Geosciences"}]}]},"item_1_creator_7":{"attribute_name":"著者名よみ","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"テラダ, クミコ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"フクダ, ヨウイチ"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"TERADA, Kumiko","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"FUKUDA, Yoichi","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_1_description_1":{"attribute_name":"ページ属性","attribute_value_mlt":[{"subitem_description":"P(論文)","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"Since the declassification of the Geosat Geodetic Mission (Geosat/GM), cross-track resolution of satellite altimeter profiles has improved remarkably. Consequently, the cross-track resolution somewhat exceeds the along-track resolution. To utilize the high-density of Geosat/GM profiles, we examine whether the along-track resolution is improved by using the 10Hz sampling data or not. For this purpose, Geosat/GM profiles in the Southern Ocean and Antarctic margin are mainly tested. Ten Hz data are converted into grids of gravity anomaly following the recipe given by D.T. SANDWELL (Geophys. J. Int., 109,437,1992). The converted grids are then compared with the grids of high-cut filtered data. The result implies that the 10 Hz data can show more detailed structures than filtered data.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00002841","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"National Institute of Polar Research"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA1072335X","subitem_source_identifier_type":"NCID"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Graduate School of Science, Kyoto University"},{"subitem_text_language":"en","subitem_text_value":"Graduate School of Science, Kyoto University"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1997-09-01"}],"displaytype":"detail","filename":"KJ00002368114.pdf","filesize":[{"value":"1.4 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002368114","url":"https://nipr.repo.nii.ac.jp/record/2841/files/KJ00002368114.pdf"},"version_id":"e2caf194-0caa-4cf2-9ef2-b7595c287311"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"altimetry","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"gravity","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Geosat/GM","subitem_subject_language":"en","subitem_subject_scheme":"Other"}]},"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":"APPLICABILITY OF 10Hz SATELLITE ALTIMETRY DATA TO THE ANTARCTIC MARGIN","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"APPLICABILITY OF 10Hz SATELLITE ALTIMETRY DATA TO THE ANTARCTIC MARGIN"}]},"item_type_id":"1","owner":"4","path":["424"],"pubdate":{"attribute_name":"公開日","attribute_value":"1997-09-01"},"publish_date":"1997-09-01","publish_status":"0","recid":"2841","relation_version_is_last":true,"title":["APPLICABILITY OF 10Hz SATELLITE ALTIMETRY DATA TO THE ANTARCTIC MARGIN"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:41:43.760757+00:00"}