WEKO3
アイテム
{"_buckets": {"deposit": "06e1df6c-d746-4ced-b8cc-ed665feeb378"}, "_deposit": {"created_by": 4, "id": "1334", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "1334"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00001334", "sets": ["378"]}, "author_link": ["4267", "1026", "139", "143"], "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1982-12", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "86", "bibliographicPageStart": "77", "bibliographicVolumeNumber": "24", "bibliographic_titles": [{"bibliographic_title": "Memoirs of National Institute of Polar Research. Special issue"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Kawaguchi, Sadao", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "143", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Kobayashi, Shun\u0027ichi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "139", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Ishikawa, Nobuyoshi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "4267", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Ohata, Tetsuo", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "1026", "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": "Aerological soundings were carried out at Mizuho Station, East Antarctica as part of POLEX-South. Surface inversions were found on all soundings from the middle of March through the middle of October. The surface inversion thickness was not larger than 500m. The thickness under clear skies was larger than that under cloudy skies. Its intensity became stronger steadily from 3℃ in February to about 20℃ in May, and then weakend gradually from July to October under clear skies, intensity under cloudy skies was weaker than under clear skies, the difference being large in winter. The temperature difference of inversion top between strong and weak cases was small : the intensities of surface inversions were determined almost entirely by the surface temperatures. Wind speeds aloft increased with height from the surface to 150m, thereafter decreased to 900m height and then increased again. The wind direction turned counterclockwise with height so as to blow parallel to the contour line of the terrain in the lowest few hundred meters in about 60% of all cases. Not only the radiative heat loss but also the air advection from the interior is important in forming the surface inversion at Mizuho Station. The surface inversions here are destroyed not merely strong wind, but by the passage of synoptic scale disturbances.", "subitem_description_type": "Other"}]}, "item_1_source_id_13": {"attribute_name": "雑誌書誌ID", "attribute_value_mlt": [{"subitem_source_identifier": "AA00733561", "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": "National Institute of Polar Research"}, {"subitem_text_language": "en", "subitem_text_value": "The Institute of Low Temperature Science, Hokkaido University"}, {"subitem_text_language": "en", "subitem_text_value": "The Institute of Low Temperature Science, Hokkaido University"}, {"subitem_text_language": "en", "subitem_text_value": "Water Research Institute, Nagoya University"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "1982-12-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00000011968.pdf", "filesize": [{"value": "1.2 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 1200000.0, "url": {"label": "KJ00000011968", "url": "https://nipr.repo.nii.ac.jp/record/1334/files/KJ00000011968.pdf"}, "version_id": "a2429113-0a9d-4a1a-af68-977462a44378"}]}, "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": "Aerological soundings of the surface boundary layer at Mizuho Station, East Antarctica", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Aerological soundings of the surface boundary layer at Mizuho Station, East Antarctica", "subitem_title_language": "en"}]}, "item_type_id": "1", "owner": "4", "path": ["378"], "permalink_uri": "https://nipr.repo.nii.ac.jp/records/1334", "pubdate": {"attribute_name": "公開日", "attribute_value": "1982-12-01"}, "publish_date": "1982-12-01", "publish_status": "0", "recid": "1334", "relation": {}, "relation_version_is_last": true, "title": ["Aerological soundings of the surface boundary layer at Mizuho Station, East Antarctica"], "weko_shared_id": 4}
Aerological soundings of the surface boundary layer at Mizuho Station, East Antarctica
https://nipr.repo.nii.ac.jp/records/1334
https://nipr.repo.nii.ac.jp/records/1334d80c3489-8835-4ef7-8588-b71d1fc9c7fa
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000011968 (1.2 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1982-12-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Aerological soundings of the surface boundary layer at Mizuho Station, East Antarctica | |||||
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 | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Kawaguchi, Sadao
× Kawaguchi, Sadao× Kobayashi, Shun'ichi× Ishikawa, Nobuyoshi× Ohata, Tetsuo |
|||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
The Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
The Institute of Low Temperature Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Aerological soundings were carried out at Mizuho Station, East Antarctica as part of POLEX-South. Surface inversions were found on all soundings from the middle of March through the middle of October. The surface inversion thickness was not larger than 500m. The thickness under clear skies was larger than that under cloudy skies. Its intensity became stronger steadily from 3℃ in February to about 20℃ in May, and then weakend gradually from July to October under clear skies, intensity under cloudy skies was weaker than under clear skies, the difference being large in winter. The temperature difference of inversion top between strong and weak cases was small : the intensities of surface inversions were determined almost entirely by the surface temperatures. Wind speeds aloft increased with height from the surface to 150m, thereafter decreased to 900m height and then increased again. The wind direction turned counterclockwise with height so as to blow parallel to the contour line of the terrain in the lowest few hundred meters in about 60% of all cases. Not only the radiative heat loss but also the air advection from the interior is important in forming the surface inversion at Mizuho Station. The surface inversions here are destroyed not merely strong wind, but by the passage of synoptic scale disturbances. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 24, p. 77-86, 発行日 1982-12 |