Simulating Storm Surge and Inundation Along the Taiwan Coast During Typhoons Fanapi in 2010 and Soulik in 2013

  • Author(s): Y. Peter Sheng, Vladimir A. Paramygin, Chuen-Teyr Terng, and Chi-Hao Chu
  • DOI: 10.3319/TAO.2016.06.13.01(Oc)
  • Keywords: Storm surge, Coastal inundation, Numerical simulation, Fanapi, Soulik, Taiwan
  • Citation: Sheng, Y. P., V. A. Paramygin, C. T. Terng, and C. H. Chu, 2016: Simulating storm surge and inundation along the Taiwan coast during typhoons Fanapi in 2010 and Soulik in 2013. Terr. Atmos. Ocean. Sci., 27, 965-979, doi: 10.3319/TAO.2016.06.13.01(Oc)
  • The surge-wave modeling system produced accurate surge and wave during typhoons
  • Wave contributed significantly to storm surge during Soulik along the NE Taiwan coast
  • 3D model yields more accurate results at where wave-surge interaction is pronounced

Taiwan is subjected to significant storm surges, waves, and coastal inundation during frequent tropical cyclones. Along the west coast, with gentler bathymetric slopes, storm surges often cause significant coastal inundation. Along the east coast with steep bathymetric slopes, waves can contribute significantly to the storm surge in the form of wave setup. To examine the importance of waves in storm surges and quantify the significance of coastal inundation, this paper presents numerical simulations of storm surge and coastal inundation during two major typhoons, Fanapi in 2010 and Soulik in 2013, which impacted the southwest and northeast coasts of Taiwan, respectively. The simulations were conducted with an integrated surge-wave modeling system using a large coastal model domain wrapped around the island of Taiwan, with a grid resolution of 50 - 300 m. During Fanapi, the simulated storm surge and coastal inundation near Kaohsiung are not as accurate as those obtained using a smaller coastal domain with finer resolution (40 - 150 m). During Soulik, the model simulations show that wave setup contributed significantly (up to 20%) to the peak storm surge along the northeast coast of Taiwan. Three-D model simulations yield more accurate water level results and significant vertical variations in horizontal velocity at stations where wave-surge interaction is more pronounced. The simulated storm surge generally agreed well with the observed data at nearly 40 stations.

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