Observations of infragravity period oscillations in a small marina

Darshani Thotagamuwage, Charitha Pattiaratchi

    Research output: Contribution to journalArticlepeer-review

    39 Citations (Scopus)

    Abstract

    We measured water levels in Two Rocks Marina, Western Australia, to investigate infragravity-period (25-300 s) oscillations and their forcing mechanisms. Spectral analyses identified four dominant oscillations in the infragravity band, which were generated through excitation of the marina's natural periods. The oscillations were present at all times, independent of the offshore conditions, indicating that they were forced by a continuous external energy source. The spectral energy of the oscillations increased by ~50 times during storm events (higher incident wave heights), in comparison to calm events (lower incident wave heights). Wave heights of oscillations within the marina were strongly correlated with offshore incident swell wave heights and reached maximum of 0.5 m. The groupiness factor of swell waves around the marina was 0.6-0.85. Bound infragravity waves associated with swell wave groups were identified as potential forcing mechanism of infragravity-period oscillations within the marina. The bound infragravity waves have broad frequency spectrum without dominant periods matched the marina's natural periods however, bound infragravity waves of periods in the proximity of the marina NOPs were adequate to generate oscillations at the NOPs of the marina. Frequencies of the oscillations were independent of the forcing frequency, and determined by the marina's geometry. © 2014 Elsevier Ltd. All rights reserved.
    Original languageEnglish
    Pages (from-to)435-445
    Number of pages11
    JournalOcean Engineering
    Volume88
    Early online date25 Jul 2014
    DOIs
    Publication statusPublished - 15 Sept 2014

    Fingerprint

    Dive into the research topics of 'Observations of infragravity period oscillations in a small marina'. Together they form a unique fingerprint.

    Cite this