Geophysical Research Letters, ISSN 0094-8276, 12/2017, Volume 44, Issue 24, pp. 12,280 - 12,288
Internal waves, which drive most ocean turbulence and add “noise” to lower‐frequency records, interact with low‐frequency current systems and topography in yet...
internal waves | PART I | ENERGY | GEOSCIENCES, MULTIDISCIPLINARY | GLOBAL PATTERNS | REDISTRIBUTION | OCEAN | GENERATION | TIDES | TURBULENT DISSIPATION | PROPAGATION | INERTIAL WAVES | Turbulence | Wave energy | Turbulent flow | Oceanic turbulence | Wave power | Continental slope | Topography (geology) | Incident waves | Fluxes | Slopes (topography) | Tides | Waves | Velocity | Variance analysis | Group velocity | Storms | Inertial waves | Topography | Internal tides | Frequency | Tidal dynamics | Kinetic energy | Tidal energy | Internal waves
internal waves | PART I | ENERGY | GEOSCIENCES, MULTIDISCIPLINARY | GLOBAL PATTERNS | REDISTRIBUTION | OCEAN | GENERATION | TIDES | TURBULENT DISSIPATION | PROPAGATION | INERTIAL WAVES | Turbulence | Wave energy | Turbulent flow | Oceanic turbulence | Wave power | Continental slope | Topography (geology) | Incident waves | Fluxes | Slopes (topography) | Tides | Waves | Velocity | Variance analysis | Group velocity | Storms | Inertial waves | Topography | Internal tides | Frequency | Tidal dynamics | Kinetic energy | Tidal energy | Internal waves
Journal Article
Journal of Fluid Mechanics, ISSN 0022-1120, 10/2017, Volume 829, pp. 280 - 303
Groups of surface gravity waves induce horizontally varying Stokes drift that drives convergence of water ahead of the group and divergence behind. The mass...
stratified flows | surface gravity waves | Internal waves | MECHANICS | internal waves | PHYSICS, FLUIDS & PLASMAS | WATER | Surface gravity waves | Divergence | Boussinesq equations | Propagation | Gravitational waves | Buoyancy | Radiation | Oceanography | Waves | Density stratification | Stokes law (fluid mechanics) | Brunt-vaisala frequency | Solutions | Pumping | Mathematical models | Coupling | Stratification | Gravity waves | Gravity | Amplitude | Gravitation | Fluctuations | Computational fluid dynamics | Flux | Dimensions | Return flow | Velocity | Surface water waves | Equations | Surface waves | Boussinesq approximation | Frequency | Drift | Energy transfer
stratified flows | surface gravity waves | Internal waves | MECHANICS | internal waves | PHYSICS, FLUIDS & PLASMAS | WATER | Surface gravity waves | Divergence | Boussinesq equations | Propagation | Gravitational waves | Buoyancy | Radiation | Oceanography | Waves | Density stratification | Stokes law (fluid mechanics) | Brunt-vaisala frequency | Solutions | Pumping | Mathematical models | Coupling | Stratification | Gravity waves | Gravity | Amplitude | Gravitation | Fluctuations | Computational fluid dynamics | Flux | Dimensions | Return flow | Velocity | Surface water waves | Equations | Surface waves | Boussinesq approximation | Frequency | Drift | Energy transfer
Journal Article
Journal of Fluid Mechanics, ISSN 0022-1120, 07/2018, Volume 846, pp. 752 - 788
This paper presents experimental and theoretical results on the internal waves emitted by a bluff body moving horizontally in a linearly stratified fluid....
Wakes | Internal waves | Stratified flows | FLUIDS | stratified flows | FIELDS | PHYSICS, FLUIDS & PLASMAS | TRANSLATING BODY | FLOW | TURBULENT WAKE | MECHANICS | REYNOLDS-NUMBER | internal waves | wakes | TOWED SPHERE | LEE WAVES | NUMERICAL-SIMULATION | Fourier transforms | Separation | Turbulent flow | Fluid flow | Velocity distribution | Towing | Waves | Defects | Brunt-vaisala frequency | Phase velocity | Bluff bodies | Mathematical models | Cylinders | Amplitude | Computational fluid dynamics | Reynolds number | Shape effects | Froude number | Velocity | Wavelength | Equations | Drag | Lee waves | Vortices | Scaling | Navier-Stokes equations | Mechanics | Mechanics of the fluids | Physics
Wakes | Internal waves | Stratified flows | FLUIDS | stratified flows | FIELDS | PHYSICS, FLUIDS & PLASMAS | TRANSLATING BODY | FLOW | TURBULENT WAKE | MECHANICS | REYNOLDS-NUMBER | internal waves | wakes | TOWED SPHERE | LEE WAVES | NUMERICAL-SIMULATION | Fourier transforms | Separation | Turbulent flow | Fluid flow | Velocity distribution | Towing | Waves | Defects | Brunt-vaisala frequency | Phase velocity | Bluff bodies | Mathematical models | Cylinders | Amplitude | Computational fluid dynamics | Reynolds number | Shape effects | Froude number | Velocity | Wavelength | Equations | Drag | Lee waves | Vortices | Scaling | Navier-Stokes equations | Mechanics | Mechanics of the fluids | Physics
Journal Article
Journal of Fluid Mechanics, ISSN 0022-1120, 02/2018, Volume 836, pp. 72 - 116
The supply of energy to the internal wave field in the ocean is, in total, sufficient to support the mixing required to maintain the stratification of the...
wave-turbulence interactions | stratified turbulence | mixing | wave–turbulence interactions | DISSIPATION | INSTABILITY | GRAVITY-WAVES | GLOBAL PATTERNS | PHYSICS, FLUIDS & PLASMAS | STABILITY | DRIVEN | MECHANICS | GENERATION | STRATIFIED SHEAR FLOWS | TURBULENT OVERTURNS | MICROSTRUCTURE | Slopes | Shear | Turbulent flow | Fluid flow | Kelvin-helmholtz instability | Waves | Density stratification | Wave breaking | Energy loss | Ocean models | Wave propagation | Energy | Surface acoustic waves | Topography | Inertial waves | Dissipation | Constraint modelling | Mathematical models | Stratification | Turbulence | Computational fluid dynamics | Ocean circulation | Velocity | Equations | Internal wave breaking | Vortices | Frequency | Instability | Models | Internal waves
wave-turbulence interactions | stratified turbulence | mixing | wave–turbulence interactions | DISSIPATION | INSTABILITY | GRAVITY-WAVES | GLOBAL PATTERNS | PHYSICS, FLUIDS & PLASMAS | STABILITY | DRIVEN | MECHANICS | GENERATION | STRATIFIED SHEAR FLOWS | TURBULENT OVERTURNS | MICROSTRUCTURE | Slopes | Shear | Turbulent flow | Fluid flow | Kelvin-helmholtz instability | Waves | Density stratification | Wave breaking | Energy loss | Ocean models | Wave propagation | Energy | Surface acoustic waves | Topography | Inertial waves | Dissipation | Constraint modelling | Mathematical models | Stratification | Turbulence | Computational fluid dynamics | Ocean circulation | Velocity | Equations | Internal wave breaking | Vortices | Frequency | Instability | Models | Internal waves
Journal Article
Deep-Sea Research Part I, ISSN 0967-0637, 01/2017, Volume 119, pp. 68 - 80
Three-dimensional dynamics of internal tides on the continental slope of the Malin Sea is studied numerically and validated with the observational data...
The Malin Sea | Bottom trapped internal waves | Baroclinic tides | FREQUENCIES | ENERGY | SHELF EDGE | OCEAN | OCEANOGRAPHY | TIDE GENERATION | BREAK | MODEL | Tidal currents | Dynamic meteorology | Analysis | Ocean energy resources | Internal waves
The Malin Sea | Bottom trapped internal waves | Baroclinic tides | FREQUENCIES | ENERGY | SHELF EDGE | OCEAN | OCEANOGRAPHY | TIDE GENERATION | BREAK | MODEL | Tidal currents | Dynamic meteorology | Analysis | Ocean energy resources | Internal waves
Journal Article
Environmental Fluid Mechanics, ISSN 1567-7419, 2/2018, Volume 18, Issue 1, pp. 149 - 171
Internal gravity waves that are generated in the open ocean have a universal frequency spectrum, called Garrett–Munk spectrum. By initializing internal waves...
Earth Sciences | Environmental Physics | Hydrology/Water Resources | Hydrogeology | Inertial oscillation | Relative dispersion | Classical Mechanics | Finite-scale Lyapunov exponent (FSLE) | Earth Sciences, general | Oceanography | Garrett–Munk spectrum | CIRCULATION | STATISTICS | DRIFTER OBSERVATIONS | TRAJECTORIES | WATER RESOURCES | GULF-OF-MEXICO | ENVIRONMENTAL SCIENCES | TRANSPORT | MECHANICS | Garrett-Munk spectrum | OCEANOGRAPHY | TURBULENCE | ADRIATIC SEA | METEOROLOGY & ATMOSPHERIC SCIENCES | SURFACE MIXED-LAYER | Analysis | Internal waves | Gravitation | Oceans | Internal gravity waves | Gravitational waves | Oscillations | Drifters | Waves | Frequency spectra | Dispersion | Mixed layer | Vortices | Inertial oscillations | Frequency spectrum | Mathematical models | Numerical experiments | Numerical models | Eddies | Gravity waves | Gravity
Earth Sciences | Environmental Physics | Hydrology/Water Resources | Hydrogeology | Inertial oscillation | Relative dispersion | Classical Mechanics | Finite-scale Lyapunov exponent (FSLE) | Earth Sciences, general | Oceanography | Garrett–Munk spectrum | CIRCULATION | STATISTICS | DRIFTER OBSERVATIONS | TRAJECTORIES | WATER RESOURCES | GULF-OF-MEXICO | ENVIRONMENTAL SCIENCES | TRANSPORT | MECHANICS | Garrett-Munk spectrum | OCEANOGRAPHY | TURBULENCE | ADRIATIC SEA | METEOROLOGY & ATMOSPHERIC SCIENCES | SURFACE MIXED-LAYER | Analysis | Internal waves | Gravitation | Oceans | Internal gravity waves | Gravitational waves | Oscillations | Drifters | Waves | Frequency spectra | Dispersion | Mixed layer | Vortices | Inertial oscillations | Frequency spectrum | Mathematical models | Numerical experiments | Numerical models | Eddies | Gravity waves | Gravity
Journal Article
JOURNAL OF PHYSICAL OCEANOGRAPHY, ISSN 0022-3670, 01/2017, Volume 47, Issue 1, pp. 181 - 198
The effects of internal waves (IWs), externally forced by high-frequency wind, on energy pathways are studied in submesoscale-resolving numerical simulations...
ANTARCTIC CIRCUMPOLAR CURRENT | WIND | INSTABILITY | OCEANOGRAPHY | ENERGETICS | GENERATION | MODEL | OCEAN INERTIAL MOTIONS | GEOSTROPHIC FLOW | MESOSCALE | BALANCE | Exchanging | Slopes | Wind | Gravitational waves | Spatial discrimination | Kinetic energy dissipation | Identification | Slopes (topography) | Waves | Loads (forces) | Pathways | Solutions | Energy | Eddy kinetic energy | Energy dissipation | Topography | Cascades | Extraction | Cyclones | Anticyclones | Mathematical models | Kinetic energy | Potential energy | Numerical simulations | Computer simulation | Ocean circulation | Fluid | Spatial analysis | Spectra | Conversion | Studies | Wavelengths | Simulation | Equivalence | Volume | Analysis | Vortices | Frequency | Mesoscale phenomena | Channel flow | Internal waves
ANTARCTIC CIRCUMPOLAR CURRENT | WIND | INSTABILITY | OCEANOGRAPHY | ENERGETICS | GENERATION | MODEL | OCEAN INERTIAL MOTIONS | GEOSTROPHIC FLOW | MESOSCALE | BALANCE | Exchanging | Slopes | Wind | Gravitational waves | Spatial discrimination | Kinetic energy dissipation | Identification | Slopes (topography) | Waves | Loads (forces) | Pathways | Solutions | Energy | Eddy kinetic energy | Energy dissipation | Topography | Cascades | Extraction | Cyclones | Anticyclones | Mathematical models | Kinetic energy | Potential energy | Numerical simulations | Computer simulation | Ocean circulation | Fluid | Spatial analysis | Spectra | Conversion | Studies | Wavelengths | Simulation | Equivalence | Volume | Analysis | Vortices | Frequency | Mesoscale phenomena | Channel flow | Internal waves
Journal Article
IEEE Journal of Oceanic Engineering, ISSN 0364-9059, 07/2017, Volume 42, Issue 3, pp. 663 - 671
Modal interferences are evident in the spectrogram of broadband signals propagated over distances and received on a single receiver. Plotted against range and...
Couplings | Time-frequency analysis | waveguide invariant | mode coupling | nonlinear internal waves | Receivers | Interference | Acoustics | Broadband communication | Intensity striation | Manganese | INTENSITY FLUCTUATIONS | INVARIANTS | FIELD | OCEAN | SHIFTS | SEA | GUIDES | ENGINEERING, ELECTRICAL & ELECTRONIC | ENGINEERING, CIVIL | SOLITONS | ENGINEERING, OCEAN | OCEANOGRAPHY | PROPAGATION | RANGE
Couplings | Time-frequency analysis | waveguide invariant | mode coupling | nonlinear internal waves | Receivers | Interference | Acoustics | Broadband communication | Intensity striation | Manganese | INTENSITY FLUCTUATIONS | INVARIANTS | FIELD | OCEAN | SHIFTS | SEA | GUIDES | ENGINEERING, ELECTRICAL & ELECTRONIC | ENGINEERING, CIVIL | SOLITONS | ENGINEERING, OCEAN | OCEANOGRAPHY | PROPAGATION | RANGE
Journal Article
Geophysical Research Letters, ISSN 0094-8276, 06/2017, Volume 44, Issue 12, pp. 6316 - 6325
Autonomous underwater gliders are conducting high-resolution surveys within the Gulf Stream along the U.S. East Coast. Glider surveys reveal two mechanisms by...
glider | lee wave | bottom mixed layer | Gulf Stream | GENERAL-CIRCULATION | HAWAIIAN RIDGE | WESTERN BOUNDARY | STRATIFIED FLOW | UPPER OCEAN | BLAKE-PLATEAU | UNDERWATER GLIDERS | GEOSCIENCES, MULTIDISCIPLINARY | FLORIDA CURRENT | NORTH-ATLANTIC | TURBULENCE | Stream flow | High resolution | Turbulent flow | Water runoff | Buoyancy | Banks (topography) | Underwater | Bathymetry | Slopes (topography) | Waves | Brunt-vaisala frequency | Energy | Topography | Vertical velocities | Plateaux | Gliders | Coastal environments | Layers | Ocean currents | Topographic features | Turbulence | Fluid dynamics | Stream discharge | Continental shelves | Topography (geology) | Rivers | Surveys | Thickness | Lee waves | Frequency | Outer continental shelf | Internal waves
glider | lee wave | bottom mixed layer | Gulf Stream | GENERAL-CIRCULATION | HAWAIIAN RIDGE | WESTERN BOUNDARY | STRATIFIED FLOW | UPPER OCEAN | BLAKE-PLATEAU | UNDERWATER GLIDERS | GEOSCIENCES, MULTIDISCIPLINARY | FLORIDA CURRENT | NORTH-ATLANTIC | TURBULENCE | Stream flow | High resolution | Turbulent flow | Water runoff | Buoyancy | Banks (topography) | Underwater | Bathymetry | Slopes (topography) | Waves | Brunt-vaisala frequency | Energy | Topography | Vertical velocities | Plateaux | Gliders | Coastal environments | Layers | Ocean currents | Topographic features | Turbulence | Fluid dynamics | Stream discharge | Continental shelves | Topography (geology) | Rivers | Surveys | Thickness | Lee waves | Frequency | Outer continental shelf | Internal waves
Journal Article
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Observations of internal waves with high sampling data of radar altimetry and MODIS images
International Journal of Remote Sensing, ISSN 0143-1161, 11/2018, Volume 39, Issue 21, pp. 7405 - 7416
The 20 Hz high sampling radar altimetry data and quasi-synchronous satellite images are applied to investigate internal waves in the South China Sea (SCS) and...
SOUTH CHINA SEA | IMAGING SCIENCE & PHOTOGRAPHIC TECHNOLOGY | REFLECTION | REMOTE SENSING | LEVEL | TOPEX | Wave height | Significant waves | Synchronous satellites | Significant wave height | Radar data | Superhigh frequencies | Altimeters | Data | Altimetry | MODIS | Satellite imagery | Phase velocity | Satellites | Wave propagation | Mathematical analysis | Modulation | C band | Radar | Radar altimetry | Radar imaging | Sampling | Internal waves
SOUTH CHINA SEA | IMAGING SCIENCE & PHOTOGRAPHIC TECHNOLOGY | REFLECTION | REMOTE SENSING | LEVEL | TOPEX | Wave height | Significant waves | Synchronous satellites | Significant wave height | Radar data | Superhigh frequencies | Altimeters | Data | Altimetry | MODIS | Satellite imagery | Phase velocity | Satellites | Wave propagation | Mathematical analysis | Modulation | C band | Radar | Radar altimetry | Radar imaging | Sampling | Internal waves
Journal Article
Journal of Fluid Mechanics, ISSN 0022-1120, 12/2018, Volume 856, pp. 898 - 920
Internal gravity wave energy contributes significantly to the energy budget of the oceans, affecting mixing and the thermohaline circulation. Hence it is...
geophysical and geological flows | stratified flows | internal waves | MECHANICS | CONVERSION | PHYSICS, FLUIDS & PLASMAS | OCEAN | TIDE GENERATION | TOPOGRAPHY | PROPAGATION | FLOW | Pycnocline | Wave power | Methodology | Laboratories | Gravitational waves | Density | Brunt-vaisala frequency | Energy budget | Energy | Light | Gravity waves | Gravity | Wave energy | Fluctuations | Oceans | Computer simulation | Computational fluid dynamics | Flux | Thermohaline circulation | Velocity | Pressure | Equations | Graphical user interface | Computer applications | Energy transfer | Methods | Internal waves | Navier-Stokes equations | Physics - Fluid Dynamics
geophysical and geological flows | stratified flows | internal waves | MECHANICS | CONVERSION | PHYSICS, FLUIDS & PLASMAS | OCEAN | TIDE GENERATION | TOPOGRAPHY | PROPAGATION | FLOW | Pycnocline | Wave power | Methodology | Laboratories | Gravitational waves | Density | Brunt-vaisala frequency | Energy budget | Energy | Light | Gravity waves | Gravity | Wave energy | Fluctuations | Oceans | Computer simulation | Computational fluid dynamics | Flux | Thermohaline circulation | Velocity | Pressure | Equations | Graphical user interface | Computer applications | Energy transfer | Methods | Internal waves | Navier-Stokes equations | Physics - Fluid Dynamics
Journal Article
Journal of Fluid Mechanics, ISSN 0022-1120, 12/2017, Volume 833, pp. 538 - 562
Here we show that monochromatic long-crested corrugations on an otherwise flat seafloor can coherently scatter the energy of an oblique incident internal wave...
topographic effects | internal waves | wave scattering | DISSIPATION | GRAVITY-WAVES | GLOBAL PATTERNS | PHYSICS, FLUIDS & PLASMAS | DEEP-OCEAN | SURFACE-WAVES | INTERFACIAL WAVES | TOPOGRAPHY | ABYSSAL OCEAN | MECHANICS | RICHARDSON-NUMBER | SCATTERING | Boussinesq equations | Gravitational waves | Banks (topography) | Chains | Incident waves | Slopes (topography) | Coherent scattering | Waves | Density stratification | Coherence length | Energy | Energy dissipation | Topography | Mathematical models | Stratification | Topographic features | Resonant interactions | Coriolis force | Topography (geology) | Ocean floor | Rotating fluids | Wavelengths | Boussinesq approximation | Frequency | Resonance | Incidence angle | Interactions | Richardson number | Internal waves | Physics - Fluid Dynamics
topographic effects | internal waves | wave scattering | DISSIPATION | GRAVITY-WAVES | GLOBAL PATTERNS | PHYSICS, FLUIDS & PLASMAS | DEEP-OCEAN | SURFACE-WAVES | INTERFACIAL WAVES | TOPOGRAPHY | ABYSSAL OCEAN | MECHANICS | RICHARDSON-NUMBER | SCATTERING | Boussinesq equations | Gravitational waves | Banks (topography) | Chains | Incident waves | Slopes (topography) | Coherent scattering | Waves | Density stratification | Coherence length | Energy | Energy dissipation | Topography | Mathematical models | Stratification | Topographic features | Resonant interactions | Coriolis force | Topography (geology) | Ocean floor | Rotating fluids | Wavelengths | Boussinesq approximation | Frequency | Resonance | Incidence angle | Interactions | Richardson number | Internal waves | Physics - Fluid Dynamics
Journal Article
Journal of Fluid Mechanics, ISSN 0022-1120, 07/2016, Volume 798, pp. 505 - 539
The internal waves (IWs) radiated by the turbulent wake of a sphere of diameter D towed at speed U are investigated using three-dimensional fully nonlinear...
wave-turbulence interactions | stratified turbulence | internal waves | GRAVITY-WAVES | PHYSICS, FLUIDS & PLASMAS | OCEAN | WAKE | SIMULATION | BEAM | PHASE CONFIGURATION | MECHANICS | SOLITARY WAVES | TOWED SPHERE | wave turbulence interactions | GENERATION | SIMILARITY | Viscosity | Enrichment | Slopes | Sea surface | Divergence | Boussinesq equations | Turbulent flow | Gravitational waves | Buoyancy | Fluid flow | Mass transport | Waves | Wave dispersion | Brunt-vaisala frequency | Wave propagation | Wavelet transforms | Turbulence | Statistical analysis | Computer simulation | Computational fluid dynamics | Reynolds number | Time series | Observers | Ocean surface | Temperature (air-sea) | Froude number | Wavelength | Wave period | Simulation | Strains | Decay | Boussinesq approximation | Visibility | Transport | Internal waves | Tracers
wave-turbulence interactions | stratified turbulence | internal waves | GRAVITY-WAVES | PHYSICS, FLUIDS & PLASMAS | OCEAN | WAKE | SIMULATION | BEAM | PHASE CONFIGURATION | MECHANICS | SOLITARY WAVES | TOWED SPHERE | wave turbulence interactions | GENERATION | SIMILARITY | Viscosity | Enrichment | Slopes | Sea surface | Divergence | Boussinesq equations | Turbulent flow | Gravitational waves | Buoyancy | Fluid flow | Mass transport | Waves | Wave dispersion | Brunt-vaisala frequency | Wave propagation | Wavelet transforms | Turbulence | Statistical analysis | Computer simulation | Computational fluid dynamics | Reynolds number | Time series | Observers | Ocean surface | Temperature (air-sea) | Froude number | Wavelength | Wave period | Simulation | Strains | Decay | Boussinesq approximation | Visibility | Transport | Internal waves | Tracers
Journal Article
Journal of Physical Oceanography, ISSN 0022-3670, 04/2018, Volume 48, Issue 4, pp. 995 - 1008
A long-term mooring array deployed in the northern Gulf of Mexico is used to analyze energy exchange between internal waves and low-frequency flows. In the...
Small scale processes | Internal waves | Inertia-gravity waves | WIND | DISSIPATION | SHEAR | PROFILES | GRAVITY-WAVES | CIRCULATION | FIELD | OCEANOGRAPHY | GENERATION | OCEAN INERTIAL MOTIONS | PROPAGATION | Exchanging | Wind | Parameters | Laboratories | Gravitational waves | Oceanography | Waves | Velocity | Wave propagation | Energy | Education | Quality control | Frequency | Energy transfer
Small scale processes | Internal waves | Inertia-gravity waves | WIND | DISSIPATION | SHEAR | PROFILES | GRAVITY-WAVES | CIRCULATION | FIELD | OCEANOGRAPHY | GENERATION | OCEAN INERTIAL MOTIONS | PROPAGATION | Exchanging | Wind | Parameters | Laboratories | Gravitational waves | Oceanography | Waves | Velocity | Wave propagation | Energy | Education | Quality control | Frequency | Energy transfer
Journal Article
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Parametric instability and wave turbulence driven by tidal excitation of internal waves
Journal of Fluid Mechanics, ISSN 0022-1120, 04/2018, Volume 840, pp. 498 - 529
We investigate the stability of stratified fluid layers undergoing homogeneous and periodic tidal deformation. We first introduce a local model which allows us...
geophysical and geological flows | stratified flows | internal waves | HOMOGENEOUS ROTATING PLANET | GRAVITY-WAVES | PHYSICS, FLUIDS & PLASMAS | GIANT PLANETS | ELLIPTIC INSTABILITY | NONLINEAR EVOLUTION | STRATIFIED TURBULENCE | 3-DIMENSIONAL INSTABILITY | MECHANICS | MIXING EFFICIENCY | FLOWS | INERTIAL WAVES | Deformation | Turbulent flow | Growth rate | Buoyancy | Fluid flow | Variations | Waves | Base flow | Fluids | Topography | Frequency spectrum | Mathematical models | Excitation | Domain names | Turbulence | Stability | Oceans | Computer simulation | Computational fluid dynamics | Deformation mechanisms | Stability analysis | Frequency spectra | Superposition (mathematics) | Studies | Rotating fluids | Frequency | Instability | Magnetic fields | Internal waves | Physics - Fluid Dynamics | Physics
geophysical and geological flows | stratified flows | internal waves | HOMOGENEOUS ROTATING PLANET | GRAVITY-WAVES | PHYSICS, FLUIDS & PLASMAS | GIANT PLANETS | ELLIPTIC INSTABILITY | NONLINEAR EVOLUTION | STRATIFIED TURBULENCE | 3-DIMENSIONAL INSTABILITY | MECHANICS | MIXING EFFICIENCY | FLOWS | INERTIAL WAVES | Deformation | Turbulent flow | Growth rate | Buoyancy | Fluid flow | Variations | Waves | Base flow | Fluids | Topography | Frequency spectrum | Mathematical models | Excitation | Domain names | Turbulence | Stability | Oceans | Computer simulation | Computational fluid dynamics | Deformation mechanisms | Stability analysis | Frequency spectra | Superposition (mathematics) | Studies | Rotating fluids | Frequency | Instability | Magnetic fields | Internal waves | Physics - Fluid Dynamics | Physics
Journal Article
JOURNAL OF FLUID MECHANICS, ISSN 0022-1120, 08/2017, Volume 824, pp. 286 - 311
We present a theoretical study of nonlinear effects that result from modal interactions in internal waves in a non-uniformly stratified finite-depth fluid with...
stratified flows | waves in rotating fluids | NEAR-INERTIAL OSCILLATIONS | PHYSICS, FLUIDS & PLASMAS | BEAMS | DEEP-OCEAN | PYCNOCLINE | MIXED-LAYER | MECHANICS | STRATIFIED FLUID | SOLITARY WAVES | GRAVITY-WAVE | internal waves | PARAMETRIC SUBHARMONIC INSTABILITY | NONLINEAR HARMONIC-GENERATION | Pycnocline | Vertical profiles | Divergence | Banks (topography) | Criteria | Slopes (topography) | Tides | Density stratification | Propagation modes | Wave propagation | Energy dissipation | Topography |
stratified flows | waves in rotating fluids | NEAR-INERTIAL OSCILLATIONS | PHYSICS, FLUIDS & PLASMAS | BEAMS | DEEP-OCEAN | PYCNOCLINE | MIXED-LAYER | MECHANICS | STRATIFIED FLUID | SOLITARY WAVES | GRAVITY-WAVE | internal waves | PARAMETRIC SUBHARMONIC INSTABILITY | NONLINEAR HARMONIC-GENERATION | Pycnocline | Vertical profiles | Divergence | Banks (topography) | Criteria | Slopes (topography) | Tides | Density stratification | Propagation modes | Wave propagation | Energy dissipation | Topography |