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internal tide
It is hypothesized that internal tide-induced variations of the sound velocity field on the shelf affect the degree of energy interaction between the first mode and the bottom.
      
Simulation of the internal tide in the Strait of Bab el Mandeb (the Red Sea)
      
Results related to simulations of the barotropic tide in the Red Sea and to the internal tide in the Strait of Bab el Mandeb are presented.
      
The geographic properties of low-frequency internal waves in the region are discussed primarily on the basis of the mechanism of internal tide generation on the continental shelfbreak, and the mechanisms of local generation and global generation.
      
Progress of studies on the internal tide generated by the passage of barotropic tide over continental shelf/slope
      
The layered model in Part I was used to simulate the internal tide in a stratified, two layer, and rectangular sea area with step-like topography.
      
The internal tide current velocities of the upper and lower layers and the interfacial elevations were computed and the effect of the upper layer water depth and density difference were studied.
      
The distributions of internal tide amplitude in interfaces were delineated.
      
The application of a finite difference model of internal tide generation to the NW European Shelf
      
A linear finite difference internal tide model has been used to predict the baroclinic stream function over a high aspect-ratio shelf slope (16∶1) with realistic topographic and density fields.
      
On the shelf the results agree with earlier observations of a mode 1 internal tide radiating towards the coast, although the predicted flux was less than expected.
      
The importance of tidal amplification and rectification as well as internal tide generation has been documented in Part I of this study.
      
local refinement along the shelf edge) grid is used to examine the influence of shelf edge grid refinement upon the internal tide generation and propagation off the west coast of Scotland.
      
The calculations show that provided that the finite element grid is refined in the internal tide generation area and the adjacent region through which the internal tide propagates, then a numerically accurate solution is obtained.
      
In the regions of strong internal tide generation with a local grid refinement, internal wave energy can accumulate at small scales and must be removed by a scale-selective filter.
      
A three-dimensional finite-element model of wind effects upon higher harmonics of the internal tide
      
A non-linear three-dimensional unstructured grid model of the M2 tide in the shelf edge area off the west coast of Scotland is used to examine the spatial distribution of the M2 internal tide and its higher harmonics in the region.
      
Tidal calculations show that there is significant small-scale spatial variability particularly in the higher harmonics of the internal tide in the region.
      
Phytoplankton photosynthetic response to light in an internal tide dominated environment
      
Depth-dependent overtides from internal tide reflection in a glacial fjord
      
 

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