Access count of this item: 104

Files in This Item:
File Description SizeFormat 
a35b1p14.pdf6.93 MBAdobe PDFView/Open
Title: 台風9119号の解析と強風の分布について
Authors: 藤井, 健  KAKEN_name
林, 泰一  KAKEN_name
光田, 寧  KAKEN_name
Author's alias: FUJII, Takeshi
HAYASHI, Taiichi
MITSUTA, Yasushi
Issue Date: 1-Apr-1992
Publisher: 京都大学防災研究所
Journal title: 京都大学防災研究所年報. B = Disaster Prevention Research Institute Annuals. B
Volume: 35
Issue: B-1
Start page: 183
End page: 191
Abstract: Typhoon 9119 (MIREILLE) making landfall at 1600 JST, Sept. 27, 1991 caused high wind disaster through Kyushu and Tohoku Districts. Characteristic features of this typhoon is investigated by pressure and wind analyses.Every ten-minute interval after landfall, pressure pattern is represented with the Schloemer's formula by the objective analysis method. In this analysis, we interporated the pressure data in the near center region of the typhoon by the time-space conversion, and the gradient wind is computed based on the computed pressure pattern.The gradient wind grew more intense after landfall and the intense wind region exceeding 50 ms-1 passed through the mountain part of Oita Prefecture and Hiroshima Bay, where the severe disasters by high wind were caused.About 2.5 hours after passing of the typhoon center, a pressure-dip with the maximum drop of 7.5 mb was observed through the northern part of Kyushu District and the western part of Chugoku District, and the life time of the dip exceeded 7.5 hours. At passing of the pressure-dip, peak gust of 20-40 ms-1 is observed, and it is considered that the investigation of this phenomenon is also important for a high wind disaster prevention work.
Appears in Collections:No.35 B-1

Show full item record

Export to RefWorks

Export Format: 

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.