当サイトでは、より良いサービスを提供するため、クッキーを利用しています。クッキーの使用に同意いただける場合は「同意」ボタンをクリックし、クッキーポリシーについては「詳細を見る」をクリックしてください。詳しくは当サイトの サイトポリシー をご確認ください。

詳細を見る...
ログイン サインアップ
言語:

WEKO3

  • トップ
  • ランキング
To

Field does not validate



インデックスリンク

インデックスツリー

  • RootNode

メールアドレスを入力してください。

WEKO

One fine body…

WEKO

One fine body…

アイテム

{"_buckets": {"deposit": "c10837e1-eb76-4d12-aca5-81d33e258788"}, "_deposit": {"id": "4475", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4475"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004475", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2004-09-15"}, "bibliographicIssueNumber": "9", "bibliographicPageEnd": "18", "bibliographicPageStart": "1", "bibliographicVolumeNumber": "109", "bibliographic_titles": [{"bibliographic_title": "Journal of Geophysical Research C: Oceans", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The interannual Indian Ocean subtropical dipole (IOSD) event, in the southern Indian Ocean is discussed using a coupled general circulation model to derive a scenario describing its complete life cycle for the first time. The positive (negative) IOSD is characterized by an anomalous warm (cool) sea surface temperature (SST) in the southwestern region of the Indian Ocean and by an anomalous cool (warm) SST in the southeastern region. The positive event brings about enhanced precipitation in the southeastern Africa during the peak phase. Composite pictures for the positive and negative IOSD clarify that an anomalous latent heat flux is the dominant factor in its formation. This flux anomaly is caused by an anomaly in the climatological wind field, which is associated with a pressure anomaly in the central region of the southern Indian Ocean. Since the flux anomaly starts during austral fall in the year previous to the event peak and develops for the next 9 months, air-sea interaction must play an active role in the formation of the IOSD. The reason the peak of the IOSD is locked to the austral summer is that the latent heat flux influences the sea surface temperature most efficiently in the austral summer when the depth of the surface mixed layer is shallowest. Copyright 2004 by the American Geophysical Union.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1029/2003JC001974"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0148-0227", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Rieko Suzuki", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Swadhin K. Behera", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Satoshi Iizuka", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Toshio Yamagata", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Indian Ocean subtropical dipole simulated using a coupled general circulation model", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Indian Ocean subtropical dipole simulated using a coupled general circulation model", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4475", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "4475", "relation": {}, "relation_version_is_last": true, "title": ["Indian Ocean subtropical dipole simulated using a coupled general circulation model"], "weko_shared_id": -1}
  1. 防災科研関係論文

Indian Ocean subtropical dipole simulated using a coupled general circulation model

https://nied-repo.bosai.go.jp/records/4475
https://nied-repo.bosai.go.jp/records/4475
10204868-4505-4412-861e-610f3412a8bd
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Indian Ocean subtropical dipole simulated using a coupled general circulation model
言語
言語 eng
著者 Rieko Suzuki

× Rieko Suzuki

en Rieko Suzuki

Search repository
Swadhin K. Behera

× Swadhin K. Behera

en Swadhin K. Behera

Search repository
Satoshi Iizuka

× Satoshi Iizuka

en Satoshi Iizuka

Search repository
Toshio Yamagata

× Toshio Yamagata

en Toshio Yamagata

Search repository
抄録
内容記述タイプ Other
内容記述 The interannual Indian Ocean subtropical dipole (IOSD) event, in the southern Indian Ocean is discussed using a coupled general circulation model to derive a scenario describing its complete life cycle for the first time. The positive (negative) IOSD is characterized by an anomalous warm (cool) sea surface temperature (SST) in the southwestern region of the Indian Ocean and by an anomalous cool (warm) SST in the southeastern region. The positive event brings about enhanced precipitation in the southeastern Africa during the peak phase. Composite pictures for the positive and negative IOSD clarify that an anomalous latent heat flux is the dominant factor in its formation. This flux anomaly is caused by an anomaly in the climatological wind field, which is associated with a pressure anomaly in the central region of the southern Indian Ocean. Since the flux anomaly starts during austral fall in the year previous to the event peak and develops for the next 9 months, air-sea interaction must play an active role in the formation of the IOSD. The reason the peak of the IOSD is locked to the austral summer is that the latent heat flux influences the sea surface temperature most efficiently in the austral summer when the depth of the surface mixed layer is shallowest. Copyright 2004 by the American Geophysical Union.
言語 en
書誌情報 en : Journal of Geophysical Research C: Oceans

巻 109, 号 9, p. 1-18
ISSN
収録物識別子タイプ ISSN
収録物識別子 0148-0227
DOI
関連識別子 10.1029/2003JC001974
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-31 01:54:31.910711
Show All versions

エクスポート

OAI-PMH
  • OAI-PMH JPCOAR
  • OAI-PMH DublinCore
  • OAI-PMH DDI
Other Formats
  • JSON
  • BIBTEX

Confirm


Powered by WEKO3

Change consent settings


Powered by WEKO3

Change consent settings