Recurrent solutions of the Alber equation initialized by Joint North Sea Wave Project spectra
Linear instability of two-dimensional wave fields and its concurrent evolution in time is here investigated by means of the Alber equation for narrow-banded random surface waves in deep water subject to inhomogeneous disturbances. The probability of freak waves in the context of these simulations is...
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Published in | Journal of fluid mechanics Vol. 719; pp. 314 - 344 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Cambridge, UK
Cambridge University Press
25.03.2013
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Subjects | |
Online Access | Get full text |
ISSN | 0022-1120 1469-7645 |
DOI | 10.1017/jfm.2013.7 |
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Abstract | Linear instability of two-dimensional wave fields and its concurrent evolution in time is here investigated by means of the Alber equation for narrow-banded random surface waves in deep water subject to inhomogeneous disturbances. The probability of freak waves in the context of these simulations is also discussed. The instability is first studied for the symmetric Lorentz spectrum, and continued for the realistic asymmetric Joint North Sea Wave Project (JONSWAP) spectrum of ocean waves with variable directional spreading and steepness. It is found that instability depends on the directional spreading and parameters
$\alpha $
and
$\gamma $
of the JONSWAP spectrum, where
$\alpha $
and
$\gamma $
are the energy scale and the peak enhancement factor, respectively. Both influence the mean steepness of waves with such a spectrum, although in different ways. Specifically, if the instability stops as a result of the directional spreading, increase of the steepness by increasing
$\alpha $
or
$\gamma $
can reactivate it. A criterion for the instability is suggested as a dimensionless ‘width parameter’,
$\Pi $
. For the unstable conditions, long-time evolution is simulated by integrating the Alber equation numerically. Recurrent evolution is obtained, which is a stochastic counterpart of the Fermi–Pasta–Ulam recurrence obtained for the cubic Schrödinger equation. This recurrence enables us to study the probability of freak waves, and the results are compared to the values given by the Rayleigh distribution. Moreover, it is found that stability–instability transition, the most unstable mode, recurrence duration and freak wave probability depend solely on the dimensionless ‘width parameter’,
$\Pi $
. |
---|---|
AbstractList | Abstract Linear instability of two-dimensional wave fields and its concurrent evolution in time is here investigated by means of the Alber equation for narrow-banded random surface waves in deep water subject to inhomogeneous disturbances. The probability of freak waves in the context of these simulations is also discussed. The instability is first studied for the symmetric Lorentz spectrum, and continued for the realistic asymmetric Joint North Sea Wave Project (JONSWAP) spectrum of ocean waves with variable directional spreading and steepness. It is found that instability depends on the directional spreading and parameters [formula omitted, refer to PDF] and [formula omitted, refer to PDF] of the JONSWAP spectrum, where [formula omitted, refer to PDF] and [formula omitted, refer to PDF] are the energy scale and the peak enhancement factor, respectively. Both influence the mean steepness of waves with such a spectrum, although in different ways. Specifically, if the instability stops as a result of the directional spreading, increase of the steepness by increasing [formula omitted, refer to PDF] or [formula omitted, refer to PDF] can reactivate it. A criterion for the instability is suggested as a dimensionless 'width parameter', [formula omitted, refer to PDF]. For the unstable conditions, long-time evolution is simulated by integrating the Alber equation numerically. Recurrent evolution is obtained, which is a stochastic counterpart of the Fermi-Pasta-Ulam recurrence obtained for the cubic Schrödinger equation. This recurrence enables us to study the probability of freak waves, and the results are compared to the values given by the Rayleigh distribution. Moreover, it is found that stability-instability transition, the most unstable mode, recurrence duration and freak wave probability depend solely on the dimensionless 'width parameter', [formula omitted, refer to PDF]. [PUBLICATION ABSTRACT] Linear instability of two-dimensional wave fields and its concurrent evolution in time is here investigated by means of the Alber equation for narrow-banded random surface waves in deep water subject to inhomogeneous disturbances. The probability of freak waves in the context of these simulations is also discussed. The instability is first studied for the symmetric Lorentz spectrum, and continued for the realistic asymmetric Joint North Sea Wave Project (JONSWAP) spectrum of ocean waves with variable directional spreading and steepness. It is found that instability depends on the directional spreading and parameters and of the JONSWAP spectrum, where and are the energy scale and the peak enhancement factor, respectively. Both influence the mean steepness of waves with such a spectrum, although in different ways. Specifically, if the instability stops as a result of the directional spreading, increase of the steepness by increasing or can reactivate it. A criterion for the instability is suggested as a dimensionless 'width parameter', . For the unstable conditions, long-time evolution is simulated by integrating the Alber equation numerically. Recurrent evolution is obtained, which is a stochastic counterpart of the Fermi-Pasta-Ulam recurrence obtained for the cubic Schrodinger equation. This recurrence enables us to study the probability of freak waves, and the results are compared to the values given by the Rayleigh distribution. Moreover, it is found that stability-instability transition, the most unstable mode, recurrence duration and freak wave probability depend solely on the dimensionless 'width parameter', . Linear instability of two-dimensional wave fields and its concurrent evolution in time is here investigated by means of the Alber equation for narrow-banded random surface waves in deep water subject to inhomogeneous disturbances. The probability of freak waves in the context of these simulations is also discussed. The instability is first studied for the symmetric Lorentz spectrum, and continued for the realistic asymmetric Joint North Sea Wave Project (JONSWAP) spectrum of ocean waves with variable directional spreading and steepness. It is found that instability depends on the directional spreading and parameters $\alpha $ and $\gamma $ of the JONSWAP spectrum, where $\alpha $ and $\gamma $ are the energy scale and the peak enhancement factor, respectively. Both influence the mean steepness of waves with such a spectrum, although in different ways. Specifically, if the instability stops as a result of the directional spreading, increase of the steepness by increasing $\alpha $ or $\gamma $ can reactivate it. A criterion for the instability is suggested as a dimensionless ‘width parameter’, $\Pi $ . For the unstable conditions, long-time evolution is simulated by integrating the Alber equation numerically. Recurrent evolution is obtained, which is a stochastic counterpart of the Fermi–Pasta–Ulam recurrence obtained for the cubic Schrödinger equation. This recurrence enables us to study the probability of freak waves, and the results are compared to the values given by the Rayleigh distribution. Moreover, it is found that stability–instability transition, the most unstable mode, recurrence duration and freak wave probability depend solely on the dimensionless ‘width parameter’, $\Pi $ . Linear instability of two-dimensional wave fields and its concurrent evolution in time is here investigated by means of the Alber equation for narrow-banded random surface waves in deep water subject to inhomogeneous disturbances. The probability of freak waves in the context of these simulations is also discussed. The instability is first studied for the symmetric Lorentz spectrum, and continued for the realistic asymmetric Joint North Sea Wave Project (JONSWAP) spectrum of ocean waves with variable directional spreading and steepness. It is found that instability depends on the directional spreading and parameters $\alpha $ and $\gamma $ of the JONSWAP spectrum, where $\alpha $ and $\gamma $ are the energy scale and the peak enhancement factor, respectively. Both influence the mean steepness of waves with such a spectrum, although in different ways. Specifically, if the instability stops as a result of the directional spreading, increase of the steepness by increasing $\alpha $ or $\gamma $ can reactivate it. A criterion for the instability is suggested as a dimensionless ‘width parameter’, $\Pi $ . For the unstable conditions, long-time evolution is simulated by integrating the Alber equation numerically. Recurrent evolution is obtained, which is a stochastic counterpart of the Fermi–Pasta–Ulam recurrence obtained for the cubic Schrödinger equation. This recurrence enables us to study the probability of freak waves, and the results are compared to the values given by the Rayleigh distribution. Moreover, it is found that stability–instability transition, the most unstable mode, recurrence duration and freak wave probability depend solely on the dimensionless ‘width parameter’, $\Pi $ . |
Author | Toffoli, A. Stiassnie, M. Ribal, A. Young, I. Babanin, A. V. |
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Cites_doi | 10.1029/2006JC004024 10.1063/1.862394 10.1103/PhysRevE.67.046305 10.1017/S0022112062000373 10.1103/PhysRev.4.345 10.1017/CBO9780511628955 10.1103/PhysRevLett.102.114502 10.1115/OMAE2011-49540 10.1071/MF96126 10.1103/PhysRevLett.105.014501 10.1017/S0022112005006312 10.1017/S0022112082000433 10.1103/PhysRevLett.86.5831 10.1016/j.physleta.2012.05.063 10.1016/0165-2125(80)90029-3 10.1103/PhysRevE.70.067302 10.1175/1520-0485(2003)33<863:NFIAFW>2.0.CO;2 10.1017/S002211201000385X 10.1098/rspa.1978.0181 10.1063/1.1453466 10.1017/S002211200900603X 10.1007/BF00913182 10.1063/1.863242 10.1175/1520-0485(1998)028<0563:FIOTOT>2.0.CO;2 10.1175/2008JPO4031.1 10.1175/2011JPO4542.1 10.1175/JPO-D-11-083.1 10.1029/2009GL041771 10.1175/2010JPO4455.1 10.1017/S0022112007009998 10.1017/S002211200999245X 10.1016/S0065-2687(08)60312-X 10.1063/1.3012542 10.1007/978-3-642-84847-6_26 10.1017/S0022112002002616 10.1016/j.euromechflu.2003.09.002 10.1017/S0022112007006507 10.1063/1.862122 10.1098/rspa.1976.0003 10.1017/CBO9780511618536 10.1017/CBO9780511736162 |
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Snippet | Linear instability of two-dimensional wave fields and its concurrent evolution in time is here investigated by means of the Alber equation for narrow-banded... Abstract Linear instability of two-dimensional wave fields and its concurrent evolution in time is here investigated by means of the Alber equation for... |
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SubjectTerms | Deep water Earth, ocean, space Evolution Exact sciences and technology External geophysics Fluid mechanics Instability Mathematical analysis Mathematical models North Sea Numerical analysis Ocean waves Physical oceanography Physics of the oceans Spreading Stability Steepness Surface waves Surface waves, tides and sea level. Seiches |
Title | Recurrent solutions of the Alber equation initialized by Joint North Sea Wave Project spectra |
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