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[PDF] Top 20 The Effect of Asymmetrical Topography on the Generation of Internal Waves.

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The Effect of Asymmetrical Topography on the Generation of Internal Waves.

The Effect of Asymmetrical Topography on the Generation of Internal Waves.

... of asymmetrical topography on internal wave energy. Internal waves are shown to be less energetic on both sides of the domain as the slope on one side becomes smaller, despite a ... See full document

79

Generation and propagation of nonlinear internal waves in Massachusetts Bay

Generation and propagation of nonlinear internal waves in Massachusetts Bay

... the generation and propagation of large internal waves in Mass Bay under different envi- ronmental ...Bay Internal Wave Experiment. According to our model, the waves observed in Mass ... See full document

19

Effect of the North Equatorial Counter Current on the generation and propagation of internal solitary waves off the Amazon shelf (SAR observations)

Effect of the North Equatorial Counter Current on the generation and propagation of internal solitary waves off the Amazon shelf (SAR observations)

... concerning Internal Waves (IWs) are often motivated by satellite observations, which have the unique ability to render their two-dimensional horizontal structure (see ... See full document

13

Generation of Vertical Fine Structure by Internal Waves in a Shear Flow

Generation of Vertical Fine Structure by Internal Waves in a Shear Flow

... (this effect was noted in [30]). For negative wave numbers, this effect is not observed but the dispersion curves are cut off in the low-frequency region which is again due to the influence of critical ... See full document

18

Effect of Plateau Length on the Transformation of Internal Solitary Waves

Effect of Plateau Length on the Transformation of Internal Solitary Waves

... Based on the laboratory experiments [5], they showed sequential images to reveal that a depression ISW propagated over a trapezoidal obstacle with a short plateau length (SL = 0.5 m) or a long ones (SL = 4.8 m). As a ... See full document

8

Generation of weakly nonlinear nonhydrostatic internal tides over large topography: a multi-modal approach

Generation of weakly nonlinear nonhydrostatic internal tides over large topography: a multi-modal approach

... nonhydrostatic internal-tide generation ...large-amplitude topography, ...the generation of higher harmonics by reflection from boundaries, ...local generation of internal ... See full document

12

Role of internal waves in the generation of nepheloid layers on the northwestern Alboran slope: Implications for continental margin shaping

Role of internal waves in the generation of nepheloid layers on the northwestern Alboran slope: Implications for continental margin shaping

... margins, internal waves have been postulated as one of the major mechanisms contributing to their formation and ...by internal waves could be large enough to resuspend sediment over ... See full document

11

The Generation and Propagation of Internal Solitary Waves in the South China Sea.

The Generation and Propagation of Internal Solitary Waves in the South China Sea.

... Analysis of the internal wave field is carried out along 20.81°N shown as the red dashed line in Fig. 1. The line is selected to cover wave generation by the two ridges in the Luzon Strait. Fig. 2 shows the ... See full document

50

Internal solitary waves: propagation, deformation and disintegration

Internal solitary waves: propagation, deformation and disintegration

... the effect that the initial wave has started to deform with formation of a trailing ...consequent generation of several positive solitary ...this internal wave transformation is shown in ... See full document

17

The effect of shear on the generation of gravity waves

The effect of shear on the generation of gravity waves

... Long’s equation (Long, 1952, 1953, 1955, 1959) models the flow of stratified incompressible fluid in two dimensions over terrain. When the base state of the flow (that is the un- perturbed flow field far upstream) is ... See full document

10

Instability in internal solitary waves with trapped cores

Instability in internal solitary waves with trapped cores

... unstable trapped cores were generated using a lock release method. The water column in the main section of the tank was seeded with tracer particles for flow visualization while that behind the lock was left unseeded. ... See full document

38

Physical Principles and Generation of Shock Waves

Physical Principles and Generation of Shock Waves

... Lorentz effect on charges in motion, the foil under- goes an explosion-like ...pressure waves into a defined focus to be placed in deeper regions of the ...shock waves are generated by a spark plug ... See full document

10

Head-on collision of internal waves with trapped cores

Head-on collision of internal waves with trapped cores

... interacting waves reaches a maximum and the kinetic energy reaches a ...Unlike waves of class (i), at this moment in time, the kinetic energy of the waves does not vanish because the flows in the ... See full document

12

The characteristics of billows generated by internal solitary waves

The characteristics of billows generated by internal solitary waves

... in waves that were broader and flatter, and the dynamics were transient in both the laboratory and the numerical ...Such waves are rare in the field, see Shroyer et ... See full document

35

Internal Tides and Internal Solitary Waves in the Northern South China Sea

Internal Tides and Internal Solitary Waves in the Northern South China Sea

... Band-pass filtered time series of zonal velocity at L1 is further compared with the temperature variations at B2, B1, and S7 (Figure 3.10). The time axis for each mooring site is shifted by the previous time lags to ... See full document

66

Generation of rogue waves at model scale

Generation of rogue waves at model scale

... rogue waves, created based on a 100-year sea state, were very similar to the New Year Wave confirming that such extreme waves, ap- proximately 25–27 m high at full scale, can indeed occur in severe sea ... See full document

13

Strongly nonlinear internal waves in near two-layer stratifications : generation, propagation and self-induced shear instabilities

Strongly nonlinear internal waves in near two-layer stratifications : generation, propagation and self-induced shear instabilities

... speed waves of substantially larger amplitude than the limiting amplitude of solitary waves can exist, and are good approximations of the corresponding Euler ...oceanic internal waves, which ... See full document

291

Transformation of surface and internal waves on a bottom step

Transformation of surface and internal waves on a bottom step

... При трансформации внутренних волн также возможен эффект прохождения падающей волны над уступом без изменения ее амплитуды, при этом |T0| = 1, но коэффициент отражения не равен нулю, а дл[r] ... See full document

17

Long solitary internal waves in stable stratifications

Long solitary internal waves in stable stratifications

... long waves are not trapped horizontally in such a ...long waves as the basic state, is ...states–travelling waves admitted by the linearized system–internal gravity waves modified by ... See full document

16

Spectral methods for internal waves: indistinguishable density profiles and double-humped solitary waves

Spectral methods for internal waves: indistinguishable density profiles and double-humped solitary waves

... observed waves often lie outside its formal domain of appli- cability, weakly nonlinear theory is commonly used to inter- pret field measurements (Moum and Smyth, 2006; Trevor- row, ...these waves in larger ... See full document

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