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Alexander V. Babanin and Brian K. Haus

the Kolmogorov interval associated with the presence of isotropic turbulence. Furthermore, magnitudes of the energy dissipation rates due to this turbulence in the particular case of 1.5-Hz deep-water waves were quantified as a function of the surface wave amplitude. The presence of such turbulence, previously not accounted for, can affect the physics of the wave energy dissipation, the subsurface boundary layer, and the ocean mixing in a significant way. The turbulence injected by breaking waves

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Sybren Drijfhout and Leo R. M. Maas

1. Introduction Near rough-bottom topography the turbulent mixing that is associated with the breaking of internal waves contributes about half of the mixing that is required to maintain the large-scale meridional overturning circulation in the ocean ( Munk and Wunsch 1998 ; Wunsch and Ferrari 2004 ). These internal waves are generated by flow over the topography; in the deep ocean, the most important source is the barotropic tide. Egbert and Ray (2001) examined the tidal dissipation by

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Johannes R. Gemmrich, Michael L. Banner, and Chris Garrett

1. Introduction Surface waves have been described as the “gearbox” between the atmosphere and ocean ( Ardhuin et al. 2005 ). In particular, wave breaking plays an important role in many air–sea exchange and upper-ocean processes. At moderate to high wind speeds the momentum transfer from wind to ocean currents passes through the wave field via wave breaking. The breaking of surface waves is responsible for the dissipation of wave energy, and thus wave breaking is a source of enhanced turbulence

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P. B. Smit and T. T. Janssen

1. Introduction The dynamics and statistics of ocean waves are important, for example, for upper-ocean dynamics (e.g., Craik and Leibovich 1976 ; Smith 2006 ; Aiki and Greatbatch 2011 ), air–sea interaction (e.g., Janssen 2009 ), ocean circulation (e.g., McWilliams and Restrepo 1999 ), and wave-driven circulation and transport processes (e.g., Hoefel and Elgar 2003 ; Svendsen 2006 ). Modern stochastic wave models are routinely applied to a wide range of oceanic scales, both in open-ocean

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Jerome A. Smith

1. Introduction Although first described over 100 years ago (e.g., Pidduck 1912 ), there has been a recent rekindling of interest in oceanic acoustic–gravity surface waves, in particular in the context of tsunamis (e.g., Stiassnie 2010 ; Kadri and Stiassnie 2012 ; Hendin and Stiassnie 2013 ; Abdolali et al. 2015 ; Cecioni et al. 2015 ). It has also been suggested that they can contribute to deep water transport ( Kadri 2014 ). The original derivation is a bit hard to follow, so in the

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Alexander V. Babanin, Jason McConochie, and Dmitry Chalikov

1. Introduction Modeling and measurements of the winds over the ocean surface are important in engineering, geophysics, remote sensing, and other metocean applications. The wind-wave/current interactions, or more generally air–sea energy and momentum exchanges, happen directly at the ocean interface, but measuring wind speeds and momentum right at the surface is difficult in field conditions, particularly at heavy seas which are usually of the main interest. Therefore, the 10-m elevation is

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S. Y. Annenkov and V. I. Shrira

1. Introduction For practical applications, it is important to know the probability of wave height in seas and oceans at a given place and time. It is essential to predict the probability density function (PDF) of surface elevations, along with the meteorological forecasting (e.g., Goda 2000 ). If a wave field is linear, it obeys the Gaussian statistics, and the wave heights follow the Rayleigh distribution, under the additional assumption of the narrowbandedness of the energy spectrum ( Rice

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Fanglou Liao and Xiao Hua Wang

important in coastal oceanic variabilities on time scales between the local inertial period and atmospheric weather changes over the continental margins ( Brink 1991 ; Ding et al. 2012 ), as they are generally excited by the alongshore wind stress ( Adams and Buchwald 1969 ). Assuming no stratification and a variable shelf bottom, the low-frequency wind-forced coastal responses generally exist as continental shelf waves (CSWs), whereas in a stratified ocean with a flat shelf bottom and a lateral

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Greg Holloway

906 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 10Oceanic Internal Waves Are Not Weak Waves GREG HOLLOWAYDepartment of Oceanography, University of Washington, Seattle 98195(Manuscript received 9 October 1979, in final form 29 February 1980)ABSTRACT It is shown that the oceanic internal wave field is too energetic' by roughly two orders of magnitudeto be treated theoretically as an assemblage of weakly interacting waves

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Dejun Dai, Fangli Qiao, Wojciech Sulisz, Lei Han, and Alexander Babanin

1. Introduction Energy input from wind to the surface waves, integrated over the World Ocean, is about 60 TW ( Wang and Huang 2004 ). Such a large amount of energy will dissipate and cause mixing in the ocean mixed layer. Qiao et al. (2004) proposed a parameterization scheme for the nonbreaking surface-wave-induced vertical mixing (NBWAIM), and numerical experiments show that this parameterization can significantly improve the performance of the ocean circulation models ( Qiao et al. 2004

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