ダウンロード数: 1

このアイテムのファイル:
このアイテムに関連するファイルはありません。
完全メタデータレコード
DCフィールド言語
dc.contributor.authorBaba, Yasuyukien
dc.contributor.authorKubo, Teruhiroen
dc.contributor.authorUchiyama, Yusukeen
dc.contributor.authorKihara, Naotoen
dc.contributor.authorMori, Nobuhitoen
dc.contributor.authorMuto, Yasunorien
dc.contributor.authorSuzuki, Takayukien
dc.date.accessioned2015-03-24T06:24:56Z-
dc.date.available2015-03-24T06:24:56Z-
dc.date.issued2013-11-
dc.identifier.urihttp://hdl.handle.net/2433/196268-
dc.descriptionInternational Association for Hydro-Environment Engineering and Research(IAHR) 35th World Congress, 8-13 September 2013, Chengdu, Chinaen
dc.description.abstractThis paper shows some results of intensive field observations carried out in the summer seasons since 2009. The intensive field observations have been conducted at the observation tower of Shirahama Oceanographic Observatory (SOO), DPRI, Kyoto University. The observation tower of SOO is an offshore platform for the oceanographic and meteorological observation and it is located at the bay mouth of Tanabe bay, the southwestern part of Kii Penisula, Japan. One of the aims of the observations is field data measurements to comprehend the vertical mixing process due to wind and wind wave. During the observations, five typhoons (Melor in 2009, Ma-on, Talas and Roke in 2011 and Jelawat in2012) hit the Kii peninsula. Three of them (Melor, Roke and Jelawat) passed along the southern coast of Japan and they have similar tracks around the Kii peninsula. Only Talas in 2011 passed across the main island of Japan and reached the Sea of Japan. In the observations, the vertical profiles of currents and water temperature have been measured as well as wind and wave conditions. The main results are as follows: Wind and wave conditions have common characteristics like the temporal variation of wave period and the incidence of high wave peak even though these conditions are affected by the typhoon tracks. The temporal variations of water temperature have also similar trends when the typhoons come close to the observation site, however, the vertical profiles of water temperature before and after the typhoon coming have big difference. The observed results underline the needs for the continuous observation activities and multidimensional data analysis combined with numerical simulations in order to investigate the mixing process under stormy conditions.en
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherTsinghua University Pressen
dc.rights未許諾のため本文は公開していません.ja
dc.subjectTyphoonen
dc.subjectField observationen
dc.subjectVertical mixingen
dc.titleField observations at an offshore observation tower during the typhoon seasonsen
dc.typejournal article-
dc.type.niitypeJournal Article-
dc.identifier.jtitleProceedings of 2013 IAHR Congressen
dc.textversionnone-
dc.identifier.artnum共同研究(一般共同研究)24G-05-
dc.sortkey03-
dc.addressShirahama Oceanographic Observatory, DPRI, Kyoto Univ.en
dc.addressShirahama Oceanographic Observatory, DPRI, Kyoto Univ.en
dc.addressDept. of Civil Engineering, Kobe Univ.en
dc.addressCentral Research Institute of Electric Power Industryen
dc.addressDPRI, Kyoto Univ.en
dc.addressDept. of Civil and Environmental Engineering, Tokushima Univ.en
dc.addressFaculty of Urban Innovation, Yokohama National Univ.en
dc.relation.urlhttp://www.iahr2013.org/-
dcterms.accessRightsmetadata only access-
出現コレクション:高潮・波浪災害リスク軽減に向けた大気-海洋-地盤系における界面力学過程に関する現地調査

アイテムの簡略レコードを表示する

Export to RefWorks


出力フォーマット 


このリポジトリに保管されているアイテムはすべて著作権により保護されています。