4.7 Article

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

Journal

GEOPHYSICAL RESEARCH LETTERS
Volume 41, Issue 14, Pages 5106-5113

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1002/2014GL060689

Keywords

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Funding

  1. Japan Society for the Promotion of Science Kakenhi grant
  2. Program for Risk Information on Climate Change of the Japanese Ministry of Education, Culture, Sports, Science, and Technology
  3. Disaster Prevention Research Institute of Kyoto University
  4. Grants-in-Aid for Scientific Research [25420522, 25289153, 24651207] Funding Source: KAKEN

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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 5-6m 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.

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