WEKO3
アイテム
{"_buckets": {"deposit": "0f587c15-5d9e-4cc6-86ee-bb12e4713792"}, "_deposit": {"created_by": 4, "id": "3878", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "3878"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00003878", "sets": ["533"]}, "author_link": ["6509", "6507", "6508", "6510", "6512", "6511", "6513", "6514"], "item_1_alternative_title_5": {"attribute_name": "論文名よみ", "attribute_value_mlt": [{"subitem_alternative_title": "HYDROLOGICAL OBSERVATIONS IN BREGGER GLACIER BASIN, SPITSBERGEN : DISCHARGE, TEMPERATURE AND ELECTRIC CONDUCTIVITY"}]}, "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1995-09", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "53", "bibliographicPageStart": "45", "bibliographicVolumeNumber": "9", "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": "コダマ, ユウジ"}], "nameIdentifiers": [{"nameIdentifier": "6507", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "タケウチ, ユカリ"}], "nameIdentifiers": [{"nameIdentifier": "6508", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "ナカバヤシ, ヒロノリ"}], "nameIdentifiers": [{"nameIdentifier": "6509", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "ワタナベ, オキツグ"}], "nameIdentifiers": [{"nameIdentifier": "6510", "nameIdentifierScheme": "WEKO"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "KODAMA, Yuji", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "6511", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "TAKEUCHI, Yukari", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "6512", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "NAKABAYASHI, Hironori", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "6513", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "WATANABE, Okitsugu", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "6514", "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": "The discharge, water temperature and specific electric conductivity (S.E.C.) of the Bayelva River near Ny Alesund, Spitsbergen, Svalbard were observed from the middle of June to the middle of August 1993. The daily mean of water temperature variation did not show a clear relationship with the discharge rate, whereas that of S. E. C. showed a good correlation with the discharge, showing increasing S.E.C. with decreasing discharge rate, except sometimes when there was a local maximum of discharge due to rainfall runoff. The mean diurnal hodographs of water temperature and S.E.C. to the discharge showed a clockwise hysteretic loop, which could be explained by the combination of the heat and soluble materials added to the stream and the proportion of glacier ice melt water and the base flow.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00003878", "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": "Institute of Low Temperature Science, Hokkaido University"}, {"subitem_text_language": "en", "subitem_text_value": "Institute of Low Temperature Science, Hokkaido University"}, {"subitem_text_language": "en", "subitem_text_value": "Institute of Low Temperature Science, Hokkaido University"}, {"subitem_text_language": "en", "subitem_text_value": "National Institute of Polar Research"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "1995-09-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00001014995.pdf", "filesize": [{"value": "962.5 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 962500.0, "url": {"label": "KJ00001014995", "url": "https://nipr.repo.nii.ac.jp/record/3878/files/KJ00001014995.pdf"}, "version_id": "8a6516cd-2512-42db-8c51-e2190019c99e"}]}, "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": "HYDROLOGICAL OBSERVATIONS IN BREGGER GLACIER BASIN, SPITSBERGEN : DISCHARGE, TEMPERATURE AND ELECTRIC CONDUCTIVITY", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "HYDROLOGICAL OBSERVATIONS IN BREGGER GLACIER BASIN, SPITSBERGEN : DISCHARGE, TEMPERATURE AND ELECTRIC CONDUCTIVITY"}]}, "item_type_id": "1", "owner": "4", "path": ["533"], "permalink_uri": "https://doi.org/10.15094/00003878", "pubdate": {"attribute_name": "公開日", "attribute_value": "1995-09-01"}, "publish_date": "1995-09-01", "publish_status": "0", "recid": "3878", "relation": {}, "relation_version_is_last": true, "title": ["HYDROLOGICAL OBSERVATIONS IN BREGGER GLACIER BASIN, SPITSBERGEN : DISCHARGE, TEMPERATURE AND ELECTRIC CONDUCTIVITY"], "weko_shared_id": 4}
HYDROLOGICAL OBSERVATIONS IN BREGGER GLACIER BASIN, SPITSBERGEN : DISCHARGE, TEMPERATURE AND ELECTRIC CONDUCTIVITY
https://doi.org/10.15094/00003878
https://doi.org/10.15094/0000387807039cb4-c16c-4ac6-ab93-f78fe3b151f2
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00001014995 (962.5 kB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1995-09-01 | |||||
タイトル | ||||||
タイトル | HYDROLOGICAL OBSERVATIONS IN BREGGER GLACIER BASIN, SPITSBERGEN : DISCHARGE, TEMPERATURE AND ELECTRIC CONDUCTIVITY | |||||
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 | 10.15094/00003878 | |||||
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) | |||||
論文名よみ | ||||||
その他のタイトル | HYDROLOGICAL OBSERVATIONS IN BREGGER GLACIER BASIN, SPITSBERGEN : DISCHARGE, TEMPERATURE AND ELECTRIC CONDUCTIVITY | |||||
著者名よみ |
コダマ, ユウジ
× コダマ, ユウジ× タケウチ, ユカリ× ナカバヤシ, ヒロノリ× ワタナベ, オキツグ |
|||||
著者名(英) |
KODAMA, Yuji
× KODAMA, Yuji× TAKEUCHI, Yukari× NAKABAYASHI, Hironori× WATANABE, Okitsugu |
|||||
著者所属(英) | ||||||
en | ||||||
Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The discharge, water temperature and specific electric conductivity (S.E.C.) of the Bayelva River near Ny Alesund, Spitsbergen, Svalbard were observed from the middle of June to the middle of August 1993. The daily mean of water temperature variation did not show a clear relationship with the discharge rate, whereas that of S. E. C. showed a good correlation with the discharge, showing increasing S.E.C. with decreasing discharge rate, except sometimes when there was a local maximum of discharge due to rainfall runoff. The mean diurnal hodographs of water temperature and S.E.C. to the discharge showed a clockwise hysteretic loop, which could be explained by the combination of the heat and soluble materials added to the stream and the proportion of glacier ice melt water and the base flow. | |||||
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 9, p. 45-53, 発行日 1995-09 |
|||||
出版者 | ||||||
出版者 | National Institute of Polar Research |