Interaction of Water Waves and Currents

Peregrine, D. H.

doi:10.1016/s0065-2156(08)70087-5

Cited by 518 publications

(356 citation statements)

References 113 publications

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“…In the case of short wave advection by long waves, with a clear scale separation, Broche et al (1983) showed that (7.2) is consistent with the theory of Weber and Barrick (1977). In remains to be proved that (7.2), or a more accurate version of it, is also consistent with the known amplitude dispersion of Stokes waves, or other theories for the dispersion of waves in a random wave field (Hayes, 1973;Willebrand, 1975;Huang and Tung, 1976;Masuda et al, 1979), short wave modulation by long waves (Phillips 1981), and finite amplitude waves over shear currents (e.g., Dalrymple, 1974;Peregrine, 1976).…”

Section: Waves Over Varying Currents Non-linear Wave Effects and Thesupporting

confidence: 70%

Wave modelling – The state of the art

Cavaleri¹,

Alves²,

Ardhuin³

et al. 2007

Progress in Oceanography

460

177

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This paper is the product of the wave modelling community and it tries to make a picture of the present situation in this branch of science, exploring the previous and the most recent results and looking ahead towards the solution of the problems we presently face. Both theory and applications are considered.The many faces of the subject imply separate discussions. This is reflected into the single sections, seven of them, each dealing with a specific topic, the whole providing a broad and solid overview of the present state of the art. After an introduction framing the problem and the approach we followed, we deal in sequence with the following subjects: (Section) 2, generation by wind; 3, non-linear interactions in deep water; 4, white-capping dissipation; 5, non-linear interactions in shallow water; 6, dissipation at the sea bottom; 7, wave propagation; 8, numerics. The two final sections, 9 and 10, summarize the present situation from a general point of view and try to look at the future developments. Keywords

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Section: Waves Over Varying Currents Non-linear Wave Effects and Thesupporting

confidence: 70%

Wave modelling – The state of the art

Cavaleri¹,

Alves²,

Ardhuin³

et al. 2007

Progress in Oceanography

460

177

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“…During the past several decades, wave-42 current interaction has been the subject of numerous research efforts. Most of them are well 43 documented in the review articles by Peregrine (1976), Jonsson (1990) as well as Thomas and 44 Klopman (1997). 45 In many practical instances the current velocity varies significantly with depth, leading to the 46 creation of a velocity profile, for example, with a wind-driven current where the magnitude of 47 which is subject to two nonlinear free surface conditions: 123…”

mentioning

confidence: 92%

Nonlinear Wave–Current Interaction in Water of Finite Depth

Liu

Lin

Tao

et al. 2016

J. Waterway, Port, Coastal, Ocean Eng.

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This version is available at https://strathprints.strath.ac.uk/62973/ Strathprints is designed to allow users to access the research output of the University of Strathclyde. Unless otherwise explicitly stated on the manuscript, Copyright © and Moral Rights for the papers on this site are retained by the individual authors and/or other copyright owners. Please check the manuscript for details of any other licences that may have been applied. You may not engage in further distribution of the material for any profitmaking activities or any commercial gain. You may freely distribute both the url (https://strathprints.strath.ac.uk/) and the content of this paper for research or private study, educational, or not-for-profit purposes without prior permission or charge.Any correspondence concerning this service should be sent to the Strathprints administrator: strathprints@strath.ac.ukThe Strathprints institutional repository (https://strathprints.strath.ac.uk) is a digital archive of University of Strathclyde research outputs. It has been developed to disseminate open access research outputs, expose data about those outputs, and enable the management and persistent access to Strathclyde's intellectual output.

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“…Siendo ésta la ecuación general (5) de la relación de dispersión en la presencia de corrientes [12].…”

Section: Interacción Ola-corrienteunclassified

Influencia de las corrientes en los campos de oleaje en el área de Bocas de Ceniza, Caribe Colombiano

Latorre¹,

Díaz²,

Lonin³

2013

Bol. Cient. CIOH

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En Colombia, el río Magdalena es una importante vía hacia el puerto de Barranquilla, uno de los principales del país. Por lo cual es de vital importancia enfocar los estudios en esta zona y en la entrada al puerto para optimizar el desarrollo de actividades de navegación marítima. El área de Bocas de Ceniza, en la desembocadura del río, está afectada por procesos hidrodinámicos y morfodinámicos cambiantes. Con el fin de determinar los efectos que se generan por la influencia de las corrientes en los campos de oleaje, se simuló un trayecto de aproximadamente 2 km desde Bocas de Ceniza hacia interior del canal. Para lo anterior, se utilizó una combinación de dos modelos numéricos: Simulating Waves Nearshore, para el oleaje, y el Hidrodinámico Bidimensional, para corrientes, bajo distintos escenarios de acuerdo con las corrientes típicas y estados de mar más frecuentes. Las corrientes en el sector por fuera de los tajamares oscilan entre 0,1 y 0,2 m/s, a diferencia del tramo de 200 m contados desde la entrada de los tajamares hacia el interior, donde las velocidades de corriente varían entre 1,2 y 1,8 m/s. Por consiguiente, se genera una variación en la altura de ola dentro del canal de acceso. Asimismo, dependiendo de las condiciones de caudal, los valores de incremento de altura de ola varían de 0,24 m a 1,3 m. Este fenómeno aún no ha sido documentado en la literatura para esta región, aunque es importante para futuros pronósticos locales y para evaluar las condiciones oceanográficas del acceso al Puerto de Barranquilla, que podrían afectar la seguridad en la navegación.

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Interaction of Water Waves and Currents

Cited by 518 publications

References 113 publications

Wave modelling – The state of the art

Wave modelling – The state of the art

Nonlinear Wave–Current Interaction in Water of Finite Depth

Influencia de las corrientes en los campos de oleaje en el área de Bocas de Ceniza, Caribe Colombiano

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