WEKO3
アイテム
{"_buckets": {"deposit": "faa5130c-728c-4031-a00c-cb6ef8fc02ae"}, "_deposit": {"created_by": 4, "id": "4001", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "4001"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00004001", "sets": ["535"]}, "author_link": ["7421", "7414", "7422", "7415", "7416", "7423", "7418", "7417", "7419", "7420"], "item_1_alternative_title_5": {"attribute_name": "論文名よみ", "attribute_value_mlt": [{"subitem_alternative_title": "ON THE SUPERCOOLED DRIZZLE OBSERVED AT INUVIK IN THE MID-WINTER SEASON (WANTS-ARCTIC; CANADA)"}]}, "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1997-11", "bibliographicIssueDateType": "Issued"}, "bibliographicPageStart": "254", "bibliographicVolumeNumber": "11", "bibliographic_titles": [{"bibliographic_title": "Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology"}]}]}, "item_1_creator_7": {"attribute_name": "著者名よみ", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "カジカワ, マサヒロ"}], "nameIdentifiers": [{"nameIdentifier": "7414", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "キクチ, カツヒロ"}], "nameIdentifiers": [{"nameIdentifier": "7415", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "アスマ, ヨシオ"}], "nameIdentifiers": [{"nameIdentifier": "7416", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "イノウエ, ユスケ"}], "nameIdentifiers": [{"nameIdentifier": "7417", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "サトウ, ノボル"}], "nameIdentifiers": [{"nameIdentifier": "7418", "nameIdentifierScheme": "WEKO"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "KAJIKAWA, Masahiro", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "7419", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "KIKUCHI, Katsuhiro", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "7420", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "ASUMA, Yoshio", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "7421", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "INOUE, Yusuke", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "7422", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "SATO, Noboru", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "7423", "nameIdentifierScheme": "WEKO"}]}]}, "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": "Supercooled drizzle was observed at Inuvik, N. W. T., Canada (68°22′N, 133°42′W) on December 20,21 and 27,1995. Meteorological conditions in which the supercooled drizzle could form under low temperatures in the mid-winter season of Arctic Canada were examined from the sounding data and data measured by a passive microwave radiometer at ground level. The following results were obtained : 1) Supercooled drizzle fell to the ground with ice pellets and frozen drops on snow crystals. 2) The maximum size of supercooled drizzle particles increased as the depth of cloud layer saturated with respect to water increased. 3) Because a layer of air temperature higher than 0℃ was not detected from the sounding data at Inuvik, melting of snow particles was impossible. It was concluded, therefore, that supercooled drizzle was formed by the collision-coalescence process below freezing temperature.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00004001", "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": "AA10756213", "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": "Faculty of Education, Akita University"}, {"subitem_text_language": "en", "subitem_text_value": "Graduate School of Science, Hokkaido University"}, {"subitem_text_language": "en", "subitem_text_value": "Graduate School of Science, Hokkaido University"}, {"subitem_text_language": "en", "subitem_text_value": "Graduate School of Science, Hokkaido University"}, {"subitem_text_language": "en", "subitem_text_value": "Science Education Institute, Osaka"}]}, "item_1_text_3": {"attribute_name": "記事種別(英)", "attribute_value_mlt": [{"subitem_text_language": "en", "subitem_text_value": "ABSTRACT"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "1997-11-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00001014964.pdf", "filesize": [{"value": "100.8 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 100800.0, "url": {"label": "KJ00001014964", "url": "https://nipr.repo.nii.ac.jp/record/4001/files/KJ00001014964.pdf"}, "version_id": "c16eaab1-56ee-4a33-bf56-9ae2b2c1a864"}]}, "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": "ON THE SUPERCOOLED DRIZZLE OBSERVED AT INUVIK IN THE MID-WINTER SEASON (WANTS-ARCTIC; CANADA)", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "ON THE SUPERCOOLED DRIZZLE OBSERVED AT INUVIK IN THE MID-WINTER SEASON (WANTS-ARCTIC; CANADA)"}]}, "item_type_id": "1", "owner": "4", "path": ["535"], "permalink_uri": "https://doi.org/10.15094/00004001", "pubdate": {"attribute_name": "公開日", "attribute_value": "1997-11-01"}, "publish_date": "1997-11-01", "publish_status": "0", "recid": "4001", "relation": {}, "relation_version_is_last": true, "title": ["ON THE SUPERCOOLED DRIZZLE OBSERVED AT INUVIK IN THE MID-WINTER SEASON (WANTS-ARCTIC; CANADA)"], "weko_shared_id": 4}
ON THE SUPERCOOLED DRIZZLE OBSERVED AT INUVIK IN THE MID-WINTER SEASON (WANTS-ARCTIC; CANADA)
https://doi.org/10.15094/00004001
https://doi.org/10.15094/0000400112b49693-e250-4a00-8be6-1992b4470448
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00001014964 (100.8 kB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1997-11-01 | |||||
タイトル | ||||||
タイトル | ON THE SUPERCOOLED DRIZZLE OBSERVED AT INUVIK IN THE MID-WINTER SEASON (WANTS-ARCTIC; CANADA) | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00004001 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
記事種別(英) | ||||||
en | ||||||
ABSTRACT | ||||||
論文名よみ | ||||||
その他のタイトル | ON THE SUPERCOOLED DRIZZLE OBSERVED AT INUVIK IN THE MID-WINTER SEASON (WANTS-ARCTIC; CANADA) | |||||
著者名よみ |
カジカワ, マサヒロ
× カジカワ, マサヒロ× キクチ, カツヒロ× アスマ, ヨシオ× イノウエ, ユスケ× サトウ, ノボル |
|||||
著者名(英) |
KAJIKAWA, Masahiro
× KAJIKAWA, Masahiro× KIKUCHI, Katsuhiro× ASUMA, Yoshio× INOUE, Yusuke× SATO, Noboru |
|||||
著者所属(英) | ||||||
en | ||||||
Faculty of Education, Akita University | ||||||
著者所属(英) | ||||||
en | ||||||
Graduate School of Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Graduate School of Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Graduate School of Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Science Education Institute, Osaka | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Supercooled drizzle was observed at Inuvik, N. W. T., Canada (68°22′N, 133°42′W) on December 20,21 and 27,1995. Meteorological conditions in which the supercooled drizzle could form under low temperatures in the mid-winter season of Arctic Canada were examined from the sounding data and data measured by a passive microwave radiometer at ground level. The following results were obtained : 1) Supercooled drizzle fell to the ground with ice pellets and frozen drops on snow crystals. 2) The maximum size of supercooled drizzle particles increased as the depth of cloud layer saturated with respect to water increased. 3) Because a layer of air temperature higher than 0℃ was not detected from the sounding data at Inuvik, melting of snow particles was impossible. It was concluded, therefore, that supercooled drizzle was formed by the collision-coalescence process below freezing temperature. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10756213 | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 巻 11, p. 254, 発行日 1997-11 |
|||||
出版者 | ||||||
出版者 | National Institute of Polar Research |