{"created":"2023-07-25T11:07:51.741905+00:00","id":11700,"links":{},"metadata":{"_buckets":{"deposit":"138345a7-732e-4b53-8b84-064845f29100"},"_deposit":{"created_by":4,"id":"11700","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"11700"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00011700","sets":["1497:1378:1527:1533"]},"author_link":["31556","31557","31558","31559","31560","16775"],"control_number":"11700","item_10005_date_7":{"attribute_name":"発表年月日","attribute_value_mlt":[{"subitem_date_issued_datetime":"2013-11-15","subitem_date_issued_type":"Issued"}]},"item_10005_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"We investigated characteristics of cloud and long-wave downward radiation during the year 2008 at Ny-Ålesund using Micro Pulse LIDAR (MPL) and the pyrgeometer in Baseline Surface Radiation Network (BSRN). We found that long-wave downward radiation was lower as cloud base height was higher on January 1, when mean cloud amount was 10.","subitem_description_type":"Abstract"}]},"item_10005_description_6":{"attribute_name":"会議概要（会議名, 開催地, 会期, 主催者等）","attribute_value_mlt":[{"subitem_description":"第4回極域科学シンポジウム\n個別セッション：[OM] 気水圏\n11月15日（金） 国立極地研究所 ３階ラウンジ","subitem_description_type":"Other"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"竹岡, 遼","creatorNameLang":"ja"},{"creatorName":"Takeoka, Haruka","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"31556","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"西中, 規実子","creatorNameLang":"ja"},{"creatorName":"Nishinaka, Kimiko","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"31557","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"井上, 梓","creatorNameLang":"ja"},{"creatorName":"Inoue, Azusa","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"31558","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"久慈, 誠","creatorNameLang":"ja"},{"creatorName":"Kuji, Makoto","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"31559","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"矢吹, 正教","creatorNameLang":"ja"},{"creatorName":"Yabuki, Masanori","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"31560","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"塩原, 匡貴","creatorNameLang":"ja"},{"creatorName":"Shiobara, Masataka","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"16775","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":"2016-04-11"}],"displaytype":"detail","filename":"OM_TakeokaHaruka_1.pdf","filesize":[{"value":"436.5 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"OM_TakeokaHaruka_1.pdf","url":"https://nipr.repo.nii.ac.jp/record/11700/files/OM_TakeokaHaruka_1.pdf"},"version_id":"bc7fda54-f233-42fc-83fa-617b44cc94f4"}]},"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":"conference output","resourceuri":"http://purl.org/coar/resource_type/c_c94f"}]},"item_title":"北極域における雲と赤外放射量の特徴","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"北極域における雲と赤外放射量の特徴","subitem_title_language":"ja"},{"subitem_title":"Characteristics of cloud and long-wave downward radiation in Arctic region","subitem_title_language":"en"}]},"item_type_id":"10005","owner":"4","path":["1533"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2016-04-11"},"publish_date":"2016-04-11","publish_status":"0","recid":"11700","relation_version_is_last":true,"title":["北極域における雲と赤外放射量の特徴"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2025-07-18T03:07:39.150669+00:00"}