Numerical modeling of return period waves based on non-linear Boussinesq wave models to support tidal flood studies in the Kedungsepur area

A number of rapid developments and negative effects of climate change in coastal areas have forced its equilibrium system. As a result, tidal floods, high waves, and storms occur more frequently. The goal of this research is to examine nearshore hydrodynamic conditions by using results from the hind...

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Bibliographic Details
Published in:IOP conference series. Earth and environmental science 2023-08, Vol.1224 (1), p.12020
Main Authors: Khoirunnisa, H, Pasma, G R, Gumbira, G
Format: Article
Language:English
Subjects:
Bathymetry
Boussinesq equations
Boussinesq wave modeling
Climate change
Climate effects
Coastal zone
Hindcasting
Kedungsepur area
Numerical models
Return period
Storms
Tidal flood
Tidal flooding
Tidal floods
Wave height
Weather forecasting
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Summary:A number of rapid developments and negative effects of climate change in coastal areas have forced its equilibrium system. As a result, tidal floods, high waves, and storms occur more frequently. The goal of this research is to examine nearshore hydrodynamic conditions by using results from the hindcasting procedure. A non-linear Boussinesq (BW) and Spectral Wave (SW) models are used in this study. The models use the manning coefficient, bathymetry data (BATNAS), significant wave height, and wave period calculated by using the hindcasting method. This research commenced by processing wind data from the European Center for Medium-Range Weather Forecasts (ECMWF) from the years 2009 to 2021 with an interval of 3 hours. Then, wave height for return periods 1-, 50- and 100-years are calculated using Gumbel and Fisher-Tippett type I distribution, respectively. The aforementioned approach produced wave heights of 4.23; 6.16; and 6.49 m for return periods 1, 50, and 100 years, respectively. By using this series of wave data, the models predicted that 1.2 m waves propagate close to the nearshore regions.
ISSN:1755-1307
1755-1315
DOI:10.1088/1755-1315/1224/1/012020