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Wave-breaking modulation by infragravity waves during an extreme typhoon
Yoshinao Matsuba1, Takenori Shimozono1, Shinji Sato2
1Department of Civil Engineering, University of Tokyo, Tokyo, Japan.
Plos One
|April 15, 2020
Summary
Extreme typhoon conditions revealed how large infragravity waves influence nearshore wave evolution. These waves alternately slowed and sped up short wave breaking, transferring energy shoreward and increasing nearshore wave height.
Area of Science:
- Coastal processes
- Oceanography
- Wave dynamics
Background:
- Typhoons generate extreme wave conditions impacting coastal areas.
- Infragravity waves play a significant role in nearshore dynamics, especially during extreme events.
- Understanding nearshore wave evolution under extreme conditions is crucial for coastal management and hazard assessment.
Purpose of the Study:
- To analyze the effect of energetic infragravity waves on the nearshore evolution of short waves during extreme typhoon conditions.
- To investigate the mechanism by which infragravity waves influence short wave breaking and energy transfer in the nearshore zone.
Main Methods:
- Collection of coastal-wave records during a strong typhoon in Japan in 2017.
- Analysis of infragravity wave characteristics and their interaction with short waves.
- Individual wave analyses to examine the impact on short wave breaking and nearshore evolution.
Main Results:
- Extreme typhoon conditions generated large infragravity waves (up to 2m) in shallow water.
- Infragravity waves caused instantaneous water-level fluctuations, alternately decelerating and accelerating short wave breaking.
- This interaction facilitated the transmission of short-wave energy to the shore, increasing nearshore wave heights.
Conclusions:
- Infragravity waves significantly impact nearshore wave characteristics and evolution under extreme conditions.
- The study provides in situ evidence of the energy transfer mechanism from short waves on infragravity wave crests to the shore.
- Findings enhance the understanding of coastal morphodynamics during extreme weather events.
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