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- W3213366863 abstract "Predicting wave runup on reef-fringed coasts using phase-resolving modelings suffers from uncertainty induced by wave randomness, spectral-width determination, and reef-surface-roughness reproduction. A multi-layer non-hydrostatic model SWASH was first validated against two physical experiments and then applied to simulate runup over coral reefs. Simulations with different wave sequences for the same wave condition indicated that infragravity swash ( R IGW ) variability was the main contributor to the extreme runup ( R 2 % ) uncertainty. R IGW was positively correlated to the off-reef incident-wave groupiness factor and the average number of waves per wave group, suggesting that prior knowledge of incident group structure could help in reducing the uncertainty of runup prediction. In ensembles with 100 simulations of different random wave sequences, the ratio of R 2 % with 5% exceedance level to R 2 % with 95% exceedance level decreased with increasing number of spectral components and approached to 1.15–1.3 with over 600 components. Runup uncertainty induced by randomly phasing did not significantly vary with spectral widths and reef-surface roughness. Runup uncertainty due to arbitrarily specifying reef-surface roughness was much more significant than the uncertainty induced by wave randomness and spectral width, suggesting that accurate reproduction of reef surface roughness has a high priority in physical and numerical modelings. • Uncertainty in runup prediction is considerable over fringing reefs. • Variability in infragravity-frequency swash is a primary source for the uncertainty. • The uncertainty reduces with incident waves generated using more frequency bins. • Incident wave-group height and length affect the infragravity-frequency swash height. • Accurate reproduction of reef surface roughness has a high priority." @default.
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- W3213366863 date "2021-12-01" @default.
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- W3213366863 title "Uncertainty of wave runup prediction on coral reef-fringed coasts using SWASH model" @default.
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- W3213366863 doi "https://doi.org/10.1016/j.oceaneng.2021.110094" @default.
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