Rogue Wave Formation in Adverse Ocean Current Gradients

Studies of the nonlinear Schrödinger (NLS) equation indicate that surface gravity waves traveling against currents of increasing strength gain energy and steepness in the process, and this can be a mechanism for rogue wave formation. Likewise, experimental studies have shown that stable wav...

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Main Authors: Michail Manolidis, Mark Orzech, Julian Simeonov
Format: Article
Language:English
Published: MDPI AG 2019-01-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/7/2/26
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spelling doaj-7883f637b3664aac89c78c6163cc1df82021-04-02T11:19:53ZengMDPI AGJournal of Marine Science and Engineering2077-13122019-01-01722610.3390/jmse7020026jmse7020026Rogue Wave Formation in Adverse Ocean Current GradientsMichail Manolidis0Mark Orzech1Julian Simeonov2Oceanography Division, Naval Research Laboratory, Code 7322, Stennis Space Center, MS 39529, USAOceanography Division, Naval Research Laboratory, Code 7322, Stennis Space Center, MS 39529, USAMarine Geosciences Division, Naval Research Laboratory, Code 7434, Stennis Space Center, MS 39529, USAStudies of the nonlinear Schr&#246;dinger (NLS) equation indicate that surface gravity waves traveling against currents of increasing strength gain energy and steepness in the process, and this can be a mechanism for rogue wave formation. Likewise, experimental studies have shown that stable wavetrains traveling against adverse currents can give rise to extreme waves. We studied this phenomenon by using computational fluid dynamics (CFD) tools, whereby the non-hydrostatic Euler equations were solved utilizing the finite volume method. Waveforms based on a JONSWAP spectrum were generated in a numerical wave tank and were made to travel against current gradients of known strength, and wave characteristics were monitored in the process. We verified that waves gain energy from the underlying flow field as they travel against current gradients, and the simulated level of energy increase was comparable to that predicted by earlier studies of the NLS equation. The computed significant wave height, <inline-formula> <math display="inline"> <semantics> <msub> <mi>H</mi> <mi>s</mi> </msub> </semantics> </math> </inline-formula>, increased substantially, and there were strong indications that the current gradients induced nonlinear wave instabilities. The simulations were used to determine a new empirical relationship that correlates changes in the current velocity to changes in the Benjamin&#8315;Feir Index (<i>BFI</i>). The empirical relationship allows for seafaring entities to predict increased risk of rogue waves ahead, based on wave and current conditions.https://www.mdpi.com/2077-1312/7/2/26rogue wavecurrent gradientsBenjamin–Feir Indexsignificant wave heightextreme wavesnonlinear Schrödinger (NLS) equation
collection DOAJ
language English
format Article
sources DOAJ
author Michail Manolidis
Mark Orzech
Julian Simeonov
spellingShingle Michail Manolidis
Mark Orzech
Julian Simeonov
Rogue Wave Formation in Adverse Ocean Current Gradients
Journal of Marine Science and Engineering
rogue wave
current gradients
Benjamin–Feir Index
significant wave height
extreme waves
nonlinear Schrödinger (NLS) equation
author_facet Michail Manolidis
Mark Orzech
Julian Simeonov
author_sort Michail Manolidis
title Rogue Wave Formation in Adverse Ocean Current Gradients
title_short Rogue Wave Formation in Adverse Ocean Current Gradients
title_full Rogue Wave Formation in Adverse Ocean Current Gradients
title_fullStr Rogue Wave Formation in Adverse Ocean Current Gradients
title_full_unstemmed Rogue Wave Formation in Adverse Ocean Current Gradients
title_sort rogue wave formation in adverse ocean current gradients
publisher MDPI AG
series Journal of Marine Science and Engineering
issn 2077-1312
publishDate 2019-01-01
description Studies of the nonlinear Schr&#246;dinger (NLS) equation indicate that surface gravity waves traveling against currents of increasing strength gain energy and steepness in the process, and this can be a mechanism for rogue wave formation. Likewise, experimental studies have shown that stable wavetrains traveling against adverse currents can give rise to extreme waves. We studied this phenomenon by using computational fluid dynamics (CFD) tools, whereby the non-hydrostatic Euler equations were solved utilizing the finite volume method. Waveforms based on a JONSWAP spectrum were generated in a numerical wave tank and were made to travel against current gradients of known strength, and wave characteristics were monitored in the process. We verified that waves gain energy from the underlying flow field as they travel against current gradients, and the simulated level of energy increase was comparable to that predicted by earlier studies of the NLS equation. The computed significant wave height, <inline-formula> <math display="inline"> <semantics> <msub> <mi>H</mi> <mi>s</mi> </msub> </semantics> </math> </inline-formula>, increased substantially, and there were strong indications that the current gradients induced nonlinear wave instabilities. The simulations were used to determine a new empirical relationship that correlates changes in the current velocity to changes in the Benjamin&#8315;Feir Index (<i>BFI</i>). The empirical relationship allows for seafaring entities to predict increased risk of rogue waves ahead, based on wave and current conditions.
topic rogue wave
current gradients
Benjamin–Feir Index
significant wave height
extreme waves
nonlinear Schrödinger (NLS) equation
url https://www.mdpi.com/2077-1312/7/2/26
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AT markorzech roguewaveformationinadverseoceancurrentgradients
AT juliansimeonov roguewaveformationinadverseoceancurrentgradients
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