4.7 Article

On kurtosis and extreme waves in crossing directional seas: a laboratory experiment

Journal

JOURNAL OF FLUID MECHANICS
Volume 876, Issue -, Pages 792-817

Publisher

CAMBRIDGE UNIV PRESS
DOI: 10.1017/jfm.2019.575

Keywords

surface gravity waves

Funding

  1. European Community [261520]
  2. MEXT/JSPS KAKENHI in Japan [19H00782]
  3. EPSRC SUPERGEN Wind Phase 2 programme in the UK [EP/H018662/1]
  4. EPSRC [EP/H018662/1] Funding Source: UKRI
  5. Grants-in-Aid for Scientific Research [19H00782] Funding Source: KAKEN

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We examine the statistical properties of extreme and rogue wave activity in crossing directional seas, to constrain the probabilistic distributions of wave heights and wave crests in complex sea states; such crossing seas alter the statistical structure of surface waves and are known to have been involved in several marine accidents. Further, we examine the relationship between the kurtosis as an indicator of nonlinearity in the spectrum and the directionality and crossing angles of the sea-state components. Experimental tests of two-component directionally spread irregular waves with varying frequency, directional spreading and component crossing angles were carried out at the Ocean Basin Laboratory in Trondheim, Norway. The results from the experiments show that wave heights are well described by a first-order (linear) statistical distribution, while for the wave crest heights several cases exceed a second-order distribution. The number of rogue waves is relatively low overall, which agrees with previous findings in directionally spread seas. The kurtosis and wave and crest height exceedance probabilities were more affected by varying the directional spreading of the components than by varying the crossing angles between components; reducing the component directional spreading increases the kurtosis and increases the exceedance probabilities. The kurtosis can be estimated quite well for two-component seas from the directional spreading using an empirical relationship based on the two-dimensional Benjamin-Feir index when the effects of bound modes are included. This result may allow forecasting of the probability of extreme waves from the directional spreading in complex sea states.

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