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AGU: Journal of Geophysical Research, Oceans

 

Keywords

  • freak waves
  • rogue waves
  • dispersive focusing
  • wave-current interaction
  • time-frequency analysis
  • Hilbert-Huang Transformation (HHT)

Index Terms

  • Oceanography: Physical: Air/sea interactions
  • Oceanography: Physical: Nearshore processes
  • Oceanography: Physical: Surface waves and tides
  • Oceanography: Physical: Upper ocean processes
Abstract
Cited By (9)
 

Abstract

Laboratory measurements of limiting freak waves on currents

Chin H. Wu

Department of Civil and Environmental Engineering, University of Wisconsin-Madison, Madison, Wisconsin, USA

Aifeng Yao

Department of Civil and Environmental Engineering, University of Wisconsin-Madison, Madison, Wisconsin, USA

The results of laboratory measurements on limiting freak waves in the presence of currents are reported. Both dispersive spatial-temporal focusing and wave-current interaction are used to generate freak waves in a partial random wave field in the presence of currents. Wave group structure, for example, spectral slope and frequency bandwidth, is found to be critical to the formation and the geometric properties of freak waves. A nondimensional spectral bandwidth is shown to well represent wave group structure and proves to be a good indicator in determining limiting freak wave characteristics. The role of a co-existing current in the freak wave formation is recognized. Experimental results confirm that a random wave field does not prevent freak wave formation due to dispersive focusing. Strong opposing currents inducing partial wave blocking significantly elevate the limiting steepness and asymmetry of freak waves. At the location where a freak wave occurs, the Fourier spectrum exhibits local energy transfer to high-frequency waves. The Hilbert-Huang spectrum, a time-frequency-amplitude spectrum, depicts both the temporal and spectral evolution of freak waves. A strong correlation between the magnitude of interwave instantaneous frequency modulation and the freak wave nonlinearity (steepness) is observed. The experimental results provide an explanation to address the occurrence and characteristic of freak waves in consideration of the onset of wave breaking.

Received 20 July 2004; accepted 11 October 2004; published 3 December 2004.

Citation: Wu, C. H., and A. Yao (2004), Laboratory measurements of limiting freak waves on currents, J. Geophys. Res., 109, C12002, doi:10.1029/2004JC002612.

Cited By

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