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The study discusses problems in the numerical modeling of axisymmetric flows of an incompressible fluid induced by a continuous vortex region or vortex sheet by means of a discrete system of vortex rings.
      
Local separation on a slender cone preceding the appearance of a vortex sheet
      
Propagation of long nonlinear waves in a ponderable fluid beneath an ice sheet
      
The aim is to develop a method of Hamiltonian formalism for the waves in the liquid beneath an ice sheet and on that basis to construct a systematic nonlinear theory.
      
Some exact solutions of the thin-sheet stamping problem
      
Calculation of wind currents in the edge zone of a sea ice sheet
      
The steady wind currents in the ocean near the edge of an ice sheet simulated by a rigid cover are studied.
      
The time-periodic motions of a liquid layer of finite depth beneath an ice sheet with a straight infinite crack having a periodic dependence on the horizontal coordinate in the direction of the crack are considered.
      
The ice sheet is simulated by a thin elastic plate.
      
The problems of plane-wave diffraction at a crack, plane-wave diffraction atN cracks in a uniform ice sheet, and plane-wave reflection from a rigid wall are solved.
      
The effect of the pre-existing state of stress of the ice sheet on the properties of the reflected waves is investigated.
      
Dynamics of a fluid sheet on a curved rigid wall with allowance for phase transformation on the free surface
      
The flow of a three-dimensional sheet on a curved wall is considered.
      
Gravity and surface tension forces act on the sheet while a droplet stream falls on its free surface.
      
The problems of steady axisymmetric motion of the sheet on cylindrical and conical surfaces are considered.
      
The impingement of small-amplitude surface waves on the edge of a solid compressed ice sheet in a basin of finite constant depth is considered.
      
Natural vibrations of a hummock ridge in an elastic ice sheet floating on the surface of an infinitely deep fluid
      
The properties of the natural vibrations of a hummock ridge in an elastic ice sheet are investigated.
      
It is shown that natural vibrations can initiate failure of the ice sheet at a certain distance from the hummock.
      
Some features of flexural-gravity wave propagation in the presence of a crack in sheet ice
      
 

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