{"created":"2023-07-25T11:06:37.168350+00:00","id":10082,"links":{},"metadata":{"_buckets":{"deposit":"52dcc5d4-bcc2-42b3-9f1d-57159d7c7eae"},"_deposit":{"created_by":17,"id":"10082","owners":[17],"pid":{"revision_id":0,"type":"depid","value":"10082"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00010082","sets":[]},"author_link":["18648","18306","18647","4055"],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2008-06","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"127","bibliographicPageStart":"121","bibliographicVolumeNumber":"2","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":"The dynamic seeding and glaciation of a mixed-phase cloud by ice crystals injected from above at Ny Ålesund, Svalbard, Norway is described using continuous lidar measurements and thermodynamic data. Glaciation of this cloud was caused by ice crystal growth and sedimentation due to the preferential differences in saturation vapor pressure over ice versus liquid water and riming. The lidar data suggest that precipitation reached the ground for nearly 4 h as a result. The symbiosis between ice and liquid water hydrometeor presence in the polar troposphere is unique. Thermal perturbations and airmass fluctuations influence microphysical cloud characteristics and radiative balance, which makes the otherwise pristine region sensitive to lower-latitude anthropogenic and biogenic influences and a focal point for observing indirect effects and their influence on climate change. The development of lidar technologies capable of continuous and autonomous measurements is yielding important datasets to study unique atmospheric phenomena.","subitem_description_type":"Abstract"}]},"item_10001_description_6":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"本論文は北極スバールバル諸島ニーオルスンにおけるライダー観測と高層ゾンデ観測データに基づき、氷晶の種まき作用による混合相雲の氷化過程について述べたものである。この観測例では、過冷却状態の水雲の上部にすでに発生していた氷雲から氷晶粒子が降り注ぎ、その種まき作用により水雲が氷化し、さらに氷と水に対する飽和蒸気圧の差に起因する氷晶の成長と沈降およびライミングによって氷化が促進する様子が示された。極地で特徴的な混合相雲の振る舞いは、その放射過程を通して極域の気候形成におよぼす影響の点でも重要視され、その詳細な物理過程を調べる上でも、ライダーによる連続観測は極めて有効である。","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":"110006914992","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.2008.04.004"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://doi.org/10.1016/j.polar.2008.04.004","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":"Campbell, James R."}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Shiobara, Masataka"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Campbell, James R.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Shiobara, Masataka","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Atmospheric sciences","subitem_subject_scheme":"Other"},{"subitem_subject":"Cloud physics","subitem_subject_scheme":"Other"},{"subitem_subject":"Lidar","subitem_subject_scheme":"Other"},{"subitem_subject":"Atmospheric sciences","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Cloud physics","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Lidar","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":"Glaciation of a mixed-phase boundary layer cloud at a coastal arctic site as depicted in continuous lidar measurements","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Glaciation of a mixed-phase boundary layer cloud at a coastal arctic site as depicted in continuous lidar measurements"},{"subitem_title":"Glaciation of a mixed-phase boundary layer cloud at a coastal arctic site as depicted in continuous lidar measurements","subitem_title_language":"en"}]},"item_type_id":"10001","owner":"17","path":["1363"],"pubdate":{"attribute_name":"公開日","attribute_value":"2014-10-15"},"publish_date":"2014-10-15","publish_status":"0","recid":"10082","relation_version_is_last":true,"title":["Glaciation of a mixed-phase boundary layer cloud at a coastal arctic site as depicted in continuous lidar measurements"],"weko_creator_id":"17","weko_shared_id":-1},"updated":"2023-07-25T16:19:55.138661+00:00"}