TY - JOUR
T1 - Destructive tsunami-like wave generated by surf beat over a coral reef during Typhoon Haiyan
AU - Roeber, Volker
AU - Bricker, Jeremy D.
N1 - Funding Information:
Prof. Kwok Fai Cheung provided resources on a computer cluster at the University of Hawaii for the BOSZ computation. Shuichi Kure facilitated the IRIDeS field surveys in the Philippines. Troy Heitmann, Seth Guikema, Celso Ferreira, Hiroshi Takagi and Maarten van Ormondt contributed useful discussions. Akane Bessho provided graphic design. This work was funded by an IRIDeS Tokutei Project grant, and by the JSPS–NSF Cooperative Program for Interdisciplinary Joint Research Projects in Hazards and Disasters, project entitled ‘Evolution of Urban Regions in Response to Recurring Disasters’.
Publisher Copyright:
© 2015 Macmillan Publishers Limited. All rights reserved.
PY - 2015/8/6
Y1 - 2015/8/6
N2 - Storm surges cause coastal inundation due to setup of the water surface resulting from atmospheric pressure, surface winds and breaking waves. Here we show that during Typhoon Haiyan, the setup generated by breaking waves near the fringing-reef-protected town of Hernani, the Philippines, oscillated with the incidence of large and small wave groups, and steepened into a tsunami-like wave that caused extensive damage and casualties. Though fringing reefs usually protect coastal communities from moderate storms, they can exacerbate flooding during strong events with energetic waves. Typical for reef-type bathymetries, a very short wave-breaking zone over the steep reef face facilitates the freeing of infragravity-period fluctuations (surf beat) with little energy loss. Since coastal flood planning relies on phase-averaged wave modelling, infragravity surges are not being accounted for. This highlights the necessity for a policy change and the adoption of phase-resolving wave models for hazard assessment in regions with fringing reefs.
AB - Storm surges cause coastal inundation due to setup of the water surface resulting from atmospheric pressure, surface winds and breaking waves. Here we show that during Typhoon Haiyan, the setup generated by breaking waves near the fringing-reef-protected town of Hernani, the Philippines, oscillated with the incidence of large and small wave groups, and steepened into a tsunami-like wave that caused extensive damage and casualties. Though fringing reefs usually protect coastal communities from moderate storms, they can exacerbate flooding during strong events with energetic waves. Typical for reef-type bathymetries, a very short wave-breaking zone over the steep reef face facilitates the freeing of infragravity-period fluctuations (surf beat) with little energy loss. Since coastal flood planning relies on phase-averaged wave modelling, infragravity surges are not being accounted for. This highlights the necessity for a policy change and the adoption of phase-resolving wave models for hazard assessment in regions with fringing reefs.
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U2 - 10.1038/ncomms8854
DO - 10.1038/ncomms8854
M3 - Article
AN - SCOPUS:84938765496
VL - 6
JO - Nature Communications
JF - Nature Communications
SN - 2041-1723
M1 - 7854
ER -