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sheet
The effect of a crack in an ice sheet on the propagation of surface flexural-gravity waves in a basin of constant depth is analyzed.
      
The ice sheet is simulated by two floating semi-infinite fragments of a thin elastic isotropic plate.
      
Problems of wave diffraction on inhomogeneities of an elastic plate were solved in [1, 2], and on a crack in the ice sheet in [3, 4].
      
Swell wave propagation in an inhomogeneous ice sheet
      
The propagation of surface waves beneath a periodically inhomogeneous ice sheet is considered.
      
Simulation of free shear flow by the continuous vortex sheet method
      
As distinct from the discrete vortex method, which forms the basis of the method proposed, the motion of a continuous vortex sheet of finite thickness is considered.
      
The equations of motion are derived on the basis of an analysis of the physical reasons for the stability of this sheet with respect to small-scale perturbations.
      
Hydraulic jump structures in the presence of an ice sheet
      
Jumps of the bore type arising in a fluid layer with an ice sheet are investigated.
      
These jump structures are considered for a determining mechanism in the form of dispersion due to the presence of an ice sheet.
      
In contrast to the regimes studied earlier, this regime, realized when a drop crosses a sheet (a layer or jet) of gas moving in isobaric space, is called shockless drop breakup.
      
Long surface capillary-gravity waves and waves beneath an elastic plate simulating an ice sheet are considered for a liquid of finite depth.
      
It is shown experimentally that an originally circular jet with a temperature greater than 4°C transforms into a thin sheet when propagating in water at a temperature of about 0°C and sinks rather than ascends.
      
The boundary layers developing on the upper and lower sides of the airfoil form a viscous mixing layer, or vortex sheet, which separates the flows downstream of the trailing edge.
      
The investigation is performed with two types of silicate glasses: the K8 optical glass irradiated with fast electrons and an industrial sheet glass with a thermally polished surface.
      
In the first two compounds, the [ZnP2O7]2- anion has the form of a sheet consisting of Zn and P oxygen-containing tetrahedra that involves only five-membered rings.
      
The kinetics of stress relaxation in commercial sheet glasses is examined.
      
Optical schemes are given of three-dimensional illumination of the region being investigated, based on the sweeping light sheet technique.
      
A Viscous Gas Flow past a Plasma Sheet Formed by a Sliding Discharge
      
 

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