WEKO3
インデックスリンク
アイテム
{"_buckets": {"deposit": "3f1de29d-988f-4bd2-86fc-69602ed4967d"}, "_deposit": {"created_by": 3, "id": "8013", "owners": [3], "pid": {"revision_id": 0, "type": "depid", "value": "8013"}, "status": "published"}, "_oai": {"id": "oai:kanazawa-u.repo.nii.ac.jp:00008013", "sets": ["936"]}, "author_link": ["11058", "11059", "11060"], "item_4_biblio_info_8": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2010-01-01", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "1", "bibliographicPageEnd": "94", "bibliographicPageStart": "75", "bibliographicVolumeNumber": "106", "bibliographic_titles": [{"bibliographic_title": "Meteorology and Atmospheric Physics"}]}]}, "item_4_description_21": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "There is a large thermal contrast between the Arabian Peninsula and India (ΔθAI) at the mature stage of the Indian summer monsoon (ISM). The forming process of ΔθAI is investigated analyzing various datasets. It forms earlier in the lower troposphere than in the middle and upper layers. The potential temperature in the lower troposphere over the west coast of India (θIW) abruptly decreases in advance of the rapid enhancement of the westerly wind over the Arabian Sea corresponding to the ISM onset. Such a process was observed for all the target years and the rapid decrease in θIW could trigger the ISM onset. The decrease in θIW had two patterns. In one case, cooler air is brought by the strong winds around a cyclone over the Arabian Sea. In another case, θIW decreases gradually by a synergy of a southwesterly wind over the Arabian Sea and the enlargement of ΔθAI. © 2009 Springer-Verlag.", "subitem_description_type": "Abstract"}]}, "item_4_description_5": {"attribute_name": "提供者所属", "attribute_value_mlt": [{"subitem_description": "金沢大学理工研究域環境デザイン学系", "subitem_description_type": "Other"}]}, "item_4_publisher_17": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "Springer Verlag"}]}, "item_4_relation_12": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type": "isVersionOf", "subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1007/s00703-009-0051-6", "subitem_relation_type_select": "DOI"}}]}, "item_4_source_id_11": {"attribute_name": "NCID", "attribute_value_mlt": [{"subitem_source_identifier": "AA10746195", "subitem_source_identifier_type": "NCID"}]}, "item_4_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0177-7971", "subitem_source_identifier_type": "ISSN"}]}, "item_4_version_type_25": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_version_resource": "http://purl.org/coar/version/c_ab4af688f83e57aa", "subitem_version_type": "AM"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Taniguchi, Kenji"}], "nameIdentifiers": [{"nameIdentifier": "11058", "nameIdentifierScheme": "WEKO"}, {"nameIdentifier": "20422321", "nameIdentifierScheme": "金沢大学研究者情報", "nameIdentifierURI": "http://ridb.kanazawa-u.ac.jp/public/detail.php?kaken=20422321"}, {"nameIdentifier": "20422321", "nameIdentifierScheme": "研究者番号", "nameIdentifierURI": "https://nrid.nii.ac.jp/nrid/1000020422321"}]}, {"creatorNames": [{"creatorName": "Rajan, Devraj"}], "nameIdentifiers": [{"nameIdentifier": "11059", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Koike, Toshio"}], "nameIdentifiers": [{"nameIdentifier": "11060", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2017-10-03"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "TE-PR-TANIGUCHI-K-75.pdf", "filesize": [{"value": "9.7 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 9700000.0, "url": {"label": "TE-PR-TANIGUCHI-K-75.pdf", "url": "https://kanazawa-u.repo.nii.ac.jp/record/8013/files/TE-PR-TANIGUCHI-K-75.pdf"}, "version_id": "e6c747cb-56fd-478b-98d8-9fe1df471b0b"}]}, "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": "Effect of the variation in the lower tropospheric temperature on the wind onset of the Indian summer monsoon", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Effect of the variation in the lower tropospheric temperature on the wind onset of the Indian summer monsoon"}]}, "item_type_id": "4", "owner": "3", "path": ["936"], "permalink_uri": "http://hdl.handle.net/2297/20353", "pubdate": {"attribute_name": "公開日", "attribute_value": "2017-10-03"}, "publish_date": "2017-10-03", "publish_status": "0", "recid": "8013", "relation": {}, "relation_version_is_last": true, "title": ["Effect of the variation in the lower tropospheric temperature on the wind onset of the Indian summer monsoon"], "weko_shared_id": -1}
Effect of the variation in the lower tropospheric temperature on the wind onset of the Indian summer monsoon
http://hdl.handle.net/2297/20353
http://hdl.handle.net/2297/203531dce5390-eedc-4f23-acbc-8e9a67d1cf53
名前 / ファイル | ライセンス | アクション |
---|---|---|
TE-PR-TANIGUCHI-K-75.pdf (9.7 MB)
|
|
Item type | 学術雑誌論文 / Journal Article(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2017-10-03 | |||||
タイトル | ||||||
タイトル | Effect of the variation in the lower tropospheric temperature on the wind onset of the Indian summer monsoon | |||||
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 | journal article | |||||
著者 |
Taniguchi, Kenji
× Taniguchi, Kenji× Rajan, Devraj× Koike, Toshio |
|||||
提供者所属 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 金沢大学理工研究域環境デザイン学系 | |||||
書誌情報 |
Meteorology and Atmospheric Physics 巻 106, 号 1, p. 75-94, 発行日 2010-01-01 |
|||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0177-7971 | |||||
NCID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10746195 | |||||
DOI | ||||||
関連タイプ | isVersionOf | |||||
識別子タイプ | DOI | |||||
関連識別子 | 10.1007/s00703-009-0051-6 | |||||
出版者 | ||||||
出版者 | Springer Verlag | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | There is a large thermal contrast between the Arabian Peninsula and India (ΔθAI) at the mature stage of the Indian summer monsoon (ISM). The forming process of ΔθAI is investigated analyzing various datasets. It forms earlier in the lower troposphere than in the middle and upper layers. The potential temperature in the lower troposphere over the west coast of India (θIW) abruptly decreases in advance of the rapid enhancement of the westerly wind over the Arabian Sea corresponding to the ISM onset. Such a process was observed for all the target years and the rapid decrease in θIW could trigger the ISM onset. The decrease in θIW had two patterns. In one case, cooler air is brought by the strong winds around a cyclone over the Arabian Sea. In another case, θIW decreases gradually by a synergy of a southwesterly wind over the Arabian Sea and the enlargement of ΔθAI. © 2009 Springer-Verlag. | |||||
著者版フラグ | ||||||
出版タイプ | AM | |||||
出版タイプResource | http://purl.org/coar/version/c_ab4af688f83e57aa |