Abstract
Breakpoint forcing is one of the major mechanisms for generation of free infragravity waves in the surf zone. Steep bed slopes, normalised to the incident sea-swell wavelength, are recognized to favor breakpoint forcing, but no study assesses the infragravity energy generated by breakpoint forcing in real conditions. We extend the breakpoint forcing model from bichromatic to spectral forcing and dimenzionalize the model output, and we estimate the sensitivity of the model to various spectral parameters on a plane beach. Steep beaches and short period waves (wind-sea) are favourable to breakpoint forcing, as expected. We also find that more energy is generated with real, multipeak, spectral forcing than with Jonswap spectra. The predicted infragravity response is consistent with observations on a barred beach suggesting breakpoint forcing is a major mechanism for the generation of free infragravity waves in the surf zone.
Original language | English |
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Title of host publication | Journal of Coastal Research |
Subtitle of host publication | Proceedings of the 14th International Coastal Symposium |
Editors | A. Vila-Concejo, D.M. Kennedy, E. Bruce, R. Jak McCarroll |
Place of Publication | USA |
Publisher | BioOne |
Pages | 836-840 |
Number of pages | 5 |
Edition | 75 |
DOIs | |
Publication status | Published - 1 Mar 2016 |
Externally published | Yes |
Event | 14th International Coastal Symposium, ICS 2016 - Coogee Beach, Australia, Sydney, Australia Duration: 6 Mar 2016 → 11 Mar 2016 https://ics2016.org/ |
Conference
Conference | 14th International Coastal Symposium, ICS 2016 |
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Abbreviated title | ICS 2016 |
Country/Territory | Australia |
City | Sydney |
Period | 6/03/16 → 11/03/16 |
Internet address |