{"created":"2023-07-25T11:06:43.035085+00:00","id":10204,"links":{},"metadata":{"_buckets":{"deposit":"8a4b23bd-2558-4787-88df-7618ec458d67"},"_deposit":{"created_by":27,"id":"10204","owners":[27],"pid":{"revision_id":0,"type":"depid","value":"10204"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00010204","sets":[]},"author_link":["19515","19513","19516","19518","19519","19522","19520","19517","19511","19512","19509","19523","19510","19514","19508","19521"],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2011-12","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"4","bibliographicPageEnd":"410","bibliographicPageStart":"399","bibliographicVolumeNumber":"5","bibliographic_titles":[{"bibliographic_title":"Polar science"},{"bibliographic_title":"Polar science","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Solid polar stratospheric cloud (PSC) layers observed by lidar and a balloon-borne optical particle counter (OPC) on 17 December 1995 are reexamined in a comparative analysis framework. The typical radius of solid particles in the observed PSC is determined through the comparative analysis to have been approximately 2.3 μm. A backward trajectory analysis for the air mass in which the solid particles were observed shows that the air mass had experienced temperatures 2–3 K below the frost point of nitric acid tri-hydrate (NAT) during the 4 days preceding the observations. The back-trajectory analysis traces the air mass back to northern Greenland and Ellesmere Island on 16 December, one day before the observations. A microphysical box model is used to investigate possible mechanisms of formation for the observed solid particles. The results of this model suggest that the solid particles formed under mesoscale temperature fluctuations associated with mountain lee wave activity induced by the relatively high terrestrial elevations of northern Greenland and Ellesmere Island.","subitem_description_type":"Abstract"}]},"item_10001_description_6":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"1995年12月17日ノルウェイ、ニーオルスンにおいてライダーとエアロゾルゾンデにより観測した固体PSCに対して、両者の比較解析を行った。検出した固体PSCの粒径(半径)は、2.3μmと推定された。PSCを含む空気塊の温度履歴解析は、検出したPSCが観測前の4日間NATの平衡温度より数K低い温度を経験していたことを示していた。また、その空気塊は、観測の1日前にグリーンランド北部、エルズミーア島上空を通過して、ニーオルスン上空に到達していた。検出した固体PSCの形成機構について検討するため、微物理BOXモデルを利用した。その結果、検出した固体PSCは、グリーンランド北部やエルズミーア島上空な どの比較的標高の高い地形の上空を通過した時に、山岳波のようなメソスケール規模の温度擾乱下で形成した可能性が強いことが示唆された。 ","subitem_description_type":"Other"}]},"item_10001_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"国立極地研究所"}]},"item_10001_relation_12":{"attribute_name":"論文ID（NAID）","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"110008750904","subitem_relation_type_select":"NAID"}}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"10.1016/j.polar.2011.08.003"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://doi.org/10.1016/j.polar.2011.08.003","subitem_relation_type_select":"DOI"}}]},"item_10001_source_id_11":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA12240481","subitem_source_identifier_type":"NCID"}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"18739652","subitem_source_identifier_type":"ISSN"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"metadata only access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_14cb"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Shiraishi, Koichi"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Hayashi, Masahiko"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Fujiwara, Motowo"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Shibata, Takashi"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Watanabe, Masaharu"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Iwasaka, Yasunobu"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Neuber, Roland"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Yamanouchi, Takashi"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Shiraishi, Koichi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Hayashi, Masahiko","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Fujiwara, Motowo","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Shibata, Takashi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Watanabe, Masaharu","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Iwasaka, Yasunobu","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Neuber, Roland","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Yamanouchi, Takashi","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Polar stratospheric clouds","subitem_subject_scheme":"Other"},{"subitem_subject":"Stratospheric aerosol","subitem_subject_scheme":"Other"},{"subitem_subject":"Lidar","subitem_subject_scheme":"Other"},{"subitem_subject":"Aerosol sonde","subitem_subject_scheme":"Other"},{"subitem_subject":"Polar stratospheric clouds","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Stratospheric aerosol","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Lidar","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Aerosol sonde","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":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Comparative analysis of measurements of stratospheric aerosol by lidar and aerosol sonde above Ny-Alesund in the winter of 1995 [Comparative analysis of lidar and OPC observations]","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Comparative analysis of measurements of stratospheric aerosol by lidar and aerosol sonde above Ny-Alesund in the winter of 1995 [Comparative analysis of lidar and OPC observations]"},{"subitem_title":"Comparative analysis of measurements of stratospheric aerosol by lidar and aerosol sonde above Ny-Alesund in the winter of 1995 [Comparative analysis of lidar and OPC observations]","subitem_title_language":"en"}]},"item_type_id":"10001","owner":"27","path":["1353"],"pubdate":{"attribute_name":"公開日","attribute_value":"2014-10-16"},"publish_date":"2014-10-16","publish_status":"0","recid":"10204","relation_version_is_last":true,"title":["Comparative analysis of measurements of stratospheric aerosol by lidar and aerosol sonde above Ny-Alesund in the winter of 1995 [Comparative analysis of lidar and OPC observations]"],"weko_creator_id":"27","weko_shared_id":27},"updated":"2023-07-25T16:21:51.081327+00:00"}