Local amplification of storm surge by Super Typhoon Haiyan in Leyte Gulf

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  • Nobuhito Mori
    Disaster Prevention Research Institute Kyoto University Uji Kyoto Japan
  • Masaya Kato
    Hydrospheric Atmospheric Research Center Nagoya University Nagoya Japan
  • Sooyoul Kim
    Graduate School of Engineering Tottori University Tottori Japan
  • Hajime Mase
    Disaster Prevention Research Institute Kyoto University Uji Kyoto Japan
  • Yoko Shibutani
    Disaster Prevention Research Institute Kyoto University Uji Kyoto Japan
  • Tetsuya Takemi
    Disaster Prevention Research Institute Kyoto University Uji Kyoto Japan
  • Kazuhisa Tsuboki
    Hydrospheric Atmospheric Research Center Nagoya University Nagoya Japan
  • Tomohiro Yasuda
    Disaster Prevention Research Institute Kyoto University Uji Kyoto Japan

書誌事項

公開日
2014-07-25
資源種別
journal article
権利情報
  • http://creativecommons.org/licenses/by-nc-nd/3.0/
DOI
  • 10.1002/2014gl060689
公開者
American Geophysical Union (AGU)

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説明

<jats:title>Abstract</jats:title><jats:p>Typhoon Haiyan, which struck the Philippines in November 2013, was an extremely intense tropical cyclone that had a catastrophic impact. The minimum central pressure of Typhoon Haiyan was 895 hPa, making it the strongest typhoon to make landfall on a major island in the western North Pacific Ocean. The characteristics of Typhoon Haiyan and its related storm surge are estimated by numerical experiments using numerical weather prediction models and a storm surge model. Based on the analysis of best hindcast results, the storm surge level was 5–6 m and local amplification of water surface elevation due to seiche was found to be significant inside Leyte Gulf. The numerical experiments show the coherent structure of the storm surge profile due to the specific bathymetry of Leyte Gulf and the Philippines Trench as a major contributor to the disaster in Tacloban. The numerical results also indicated the sensitivity of storm surge forecast.</jats:p>

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