ログイン サインアップ
言語:

WEKO3

  • トップ
  • ランキング
To
lat lon distance
To

Field does not validate



インデックスリンク

インデックスツリー

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": "98e2dab8-1bbb-4096-b071-95ffa6502b0c"}, "_deposit": {"id": "4081", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4081"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004081", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2014-10"}, "bibliographicIssueNumber": "4", "bibliographicPageEnd": "909", "bibliographicPageStart": "898", "bibliographicVolumeNumber": "21", "bibliographic_titles": [{"bibliographic_title": "METEOROLOGICAL APPLICATIONS", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "During 11June (CASE I) and 12June (CASE II)2007, several meso--scale convective systems (MCSs) were generated along the Meiyu-Baiu front. In this study, the formation, evolution and dissipation of convective precipitation, kinematics structures, and features of the MCSs developed over ocean were investigate using dual Doppler analysis. The analysis of synoptic conditions and atmospheric sounding suggested that in both cases the atmospheric environment was characterized by well-developed convective systems with warm and humid air-inflow and unstable conditions in addition to strong vertical wind shear at lower levels. In CASEI, an embedded-cell storm developed, approached the area, and moved slowly (2.5m s(-1)) northeastward. As the system advanced, strong dominant updraft could be observed at the core. After the system passage, the wind became weak at the centre of the cell, whereas the downdraft area extended up to 4km in height on the front side. This downdraft flowed back into the convective cell and, maintained the convective activity. The evolution of the updraft and downdraft was in good agreement with the general life cycle of convective systems. In CASE II, line-shaped convective systems (LSCSs) passed from the southwest to east-northeast at 10m s(-1). The dual Doppler analysis revealed that the wind at the rear of the band contributed to the cells merge and developed into a strong convective cell. In addition, the outflow from the new cell flowed into the rear of a merged convective cell and enhanced the vertical development of the cell.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "WILEY-BLACKWELL", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1002/met.1427"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "1469-8080", "subitem_source_identifier_type": "EISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Sang-Min Jang", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Dong-In Lee", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Jong-Hoon Jeong", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Sung-Hwa Park", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Shingo Shimizu", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Hiroshi Uyeda", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Young-Sang Suh", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Radar reflectivity and wind fields analysis by using two X-band Doppler radars at Okinawa, Japan from 11 to 12 June 2007", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Radar reflectivity and wind fields analysis by using two X-band Doppler radars at Okinawa, Japan from 11 to 12 June 2007", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4081", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "4081", "relation": {}, "relation_version_is_last": true, "title": ["Radar reflectivity and wind fields analysis by using two X-band Doppler radars at Okinawa, Japan from 11 to 12 June 2007"], "weko_shared_id": -1}
  1. 防災科研関係論文

Radar reflectivity and wind fields analysis by using two X-band Doppler radars at Okinawa, Japan from 11 to 12 June 2007

https://nied-repo.bosai.go.jp/records/4081
https://nied-repo.bosai.go.jp/records/4081
a7f9136a-86d2-41c7-8cbe-5b715c350867
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Radar reflectivity and wind fields analysis by using two X-band Doppler radars at Okinawa, Japan from 11 to 12 June 2007
言語
言語 eng
著者 Sang-Min Jang

× Sang-Min Jang

en Sang-Min Jang

Search repository
Dong-In Lee

× Dong-In Lee

en Dong-In Lee

Search repository
Jong-Hoon Jeong

× Jong-Hoon Jeong

en Jong-Hoon Jeong

Search repository
Sung-Hwa Park

× Sung-Hwa Park

en Sung-Hwa Park

Search repository
Shingo Shimizu

× Shingo Shimizu

en Shingo Shimizu

Search repository
Hiroshi Uyeda

× Hiroshi Uyeda

en Hiroshi Uyeda

Search repository
Young-Sang Suh

× Young-Sang Suh

en Young-Sang Suh

Search repository
抄録
内容記述タイプ Other
内容記述 During 11June (CASE I) and 12June (CASE II)2007, several meso--scale convective systems (MCSs) were generated along the Meiyu-Baiu front. In this study, the formation, evolution and dissipation of convective precipitation, kinematics structures, and features of the MCSs developed over ocean were investigate using dual Doppler analysis. The analysis of synoptic conditions and atmospheric sounding suggested that in both cases the atmospheric environment was characterized by well-developed convective systems with warm and humid air-inflow and unstable conditions in addition to strong vertical wind shear at lower levels. In CASEI, an embedded-cell storm developed, approached the area, and moved slowly (2.5m s(-1)) northeastward. As the system advanced, strong dominant updraft could be observed at the core. After the system passage, the wind became weak at the centre of the cell, whereas the downdraft area extended up to 4km in height on the front side. This downdraft flowed back into the convective cell and, maintained the convective activity. The evolution of the updraft and downdraft was in good agreement with the general life cycle of convective systems. In CASE II, line-shaped convective systems (LSCSs) passed from the southwest to east-northeast at 10m s(-1). The dual Doppler analysis revealed that the wind at the rear of the band contributed to the cells merge and developed into a strong convective cell. In addition, the outflow from the new cell flowed into the rear of a merged convective cell and enhanced the vertical development of the cell.
言語 en
書誌情報 en : METEOROLOGICAL APPLICATIONS

巻 21, 号 4, p. 898-909
出版者
言語 en
出版者 WILEY-BLACKWELL
ISSN
収録物識別子タイプ EISSN
収録物識別子 1469-8080
DOI
関連識別子 10.1002/met.1427
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-31 01:44:03.718519
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