Occurrence of extreme waves in three-dimensional mechanically generated wave fields propagating over an oblique current

Laboratory experiments were performed to study the dynamics of three- dimensional mechanically generated waves propagating over an oblique current in partial opposition. The flow velocity varied along the mean wave direction of propagation with an increasing trend between the wave-maker and the cent...

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Main Authors: A. Toffoli, L. Cavaleri, A. V. Babanin, M. Benoit, E. M. Bitner-Gregersen, J. Monbaliu, M. Onorato, A. R. Osborne, C. T. Stansberg
Format: Article
Language:English
Published: Copernicus Publications 2011-03-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/11/895/2011/nhess-11-895-2011.pdf
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spelling doaj-d8310c80b3294b51ba9c3401eac2a6af2020-11-24T23:46:49ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812011-03-0111389590310.5194/nhess-11-895-2011Occurrence of extreme waves in three-dimensional mechanically generated wave fields propagating over an oblique currentA. ToffoliL. CavaleriA. V. BabaninM. BenoitE. M. Bitner-GregersenJ. MonbaliuM. OnoratoA. R. OsborneC. T. StansbergLaboratory experiments were performed to study the dynamics of three- dimensional mechanically generated waves propagating over an oblique current in partial opposition. The flow velocity varied along the mean wave direction of propagation with an increasing trend between the wave-maker and the centre of the tank. Tests with regular wave packets traversing the area of positive current gradient showed that the concurrent increase of wave steepness triggered modulational instability on otherwise stable wave trains and hence induced the development of very large amplitude waves. In random directional wave fields, the presence of the oblique current resulted in a weak reinforcement of wave instability with a subsequent increase of the probability of occurrence of extreme events. This seems to partially compensate the suppression of strongly non-Gaussian properties due to directional energy distribution.http://www.nat-hazards-earth-syst-sci.net/11/895/2011/nhess-11-895-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Toffoli
L. Cavaleri
A. V. Babanin
M. Benoit
E. M. Bitner-Gregersen
J. Monbaliu
M. Onorato
A. R. Osborne
C. T. Stansberg
spellingShingle A. Toffoli
L. Cavaleri
A. V. Babanin
M. Benoit
E. M. Bitner-Gregersen
J. Monbaliu
M. Onorato
A. R. Osborne
C. T. Stansberg
Occurrence of extreme waves in three-dimensional mechanically generated wave fields propagating over an oblique current
Natural Hazards and Earth System Sciences
author_facet A. Toffoli
L. Cavaleri
A. V. Babanin
M. Benoit
E. M. Bitner-Gregersen
J. Monbaliu
M. Onorato
A. R. Osborne
C. T. Stansberg
author_sort A. Toffoli
title Occurrence of extreme waves in three-dimensional mechanically generated wave fields propagating over an oblique current
title_short Occurrence of extreme waves in three-dimensional mechanically generated wave fields propagating over an oblique current
title_full Occurrence of extreme waves in three-dimensional mechanically generated wave fields propagating over an oblique current
title_fullStr Occurrence of extreme waves in three-dimensional mechanically generated wave fields propagating over an oblique current
title_full_unstemmed Occurrence of extreme waves in three-dimensional mechanically generated wave fields propagating over an oblique current
title_sort occurrence of extreme waves in three-dimensional mechanically generated wave fields propagating over an oblique current
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2011-03-01
description Laboratory experiments were performed to study the dynamics of three- dimensional mechanically generated waves propagating over an oblique current in partial opposition. The flow velocity varied along the mean wave direction of propagation with an increasing trend between the wave-maker and the centre of the tank. Tests with regular wave packets traversing the area of positive current gradient showed that the concurrent increase of wave steepness triggered modulational instability on otherwise stable wave trains and hence induced the development of very large amplitude waves. In random directional wave fields, the presence of the oblique current resulted in a weak reinforcement of wave instability with a subsequent increase of the probability of occurrence of extreme events. This seems to partially compensate the suppression of strongly non-Gaussian properties due to directional energy distribution.
url http://www.nat-hazards-earth-syst-sci.net/11/895/2011/nhess-11-895-2011.pdf
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