10 research outputs found
Propagation of acoustic-gravity waves in inhomogeneous ocean environment based on modal expansions and HP-FEM
A coupled mode model is presented for the propagation of acoustic-gravity waves
in layered ocean waveguides. The analysis extends previous work for acoustic waves in
inhomogeneous environment. The coupled mode system is derived by means of a variational
principle in conjunction with local mode series expansion, obtained by utilizing eigenfunction
systems defined in the vertical section. These are obtained through the solution of vertical
eigenvalue problems formulated along the waveguide. A crucial factor is the inclusion of
additional modes accounting for the effects of spatialy varying boundaries and interfaces. This
enhancement provides an implicit summation for the slowly convergent part of the localmode
series, rendering the series rapidly convergent, increasing substantialy the efficiency of
the method. Particular aspects of the method include high order Lagrange Finite Element
Methods for the solution of local vertical eigenvalue problems in the case of multilayered
waveguides, and Gauss-type quadrature for the computation of the coupled-mode system
coefficients. The above aspects make the present method quite efficient for long range
propagation in extended waveguides, such as the ones found in geophysical applications, e.g.
ocean basins, as only few modes are needed for the accurate representation of the wave field
Development and study of Green's function for water waves over variable bathymetry domains
Hamiltonian Variational Formulation of Three-Dimensional, Rotational Free-Surface Flows, with a Moving Seabed, in the Eulerian Description
Hamiltonian variational principles have provided, since the 1960s, the means of developing very successful wave theories for nonlinear free-surface flows, under the assumption of irrotationality. This success, in conjunction with the recognition that almost all flows in the sea are not irrotational, raises the question of extending Hamiltonâs principle to rotational free-surface flows. The Euler equations governing the bulk fluid motion have been derived by means of Hamiltonâs principle since the late 1950s. Nevertheless, a complete variational formulation of the rotational water-wave problem, including the derivation of the free-surface boundary conditions, seems to be lacking until now. The purpose of the present work is to construct such a missing variational formulation. The appropriate functional is the usual Hamiltonâs action, constrained by the conservation of mass and the conservation of fluid parcelsâ identity. The differential equations governing the bulk fluid motion are derived as usually, applying standard methods of the calculus of variations. However, the standard methodology does not provide enough structure to obtain the free-surface boundary conditions. To overcome this difficulty, differential-variational forms of the aforementioned constraints are introduced and applied to the boundary variations of the Eulerian fields. Under this transformation, both kinematic and dynamic free-surface conditions are naturally derived, ensuring the Hamiltonian variational formulation of the complete problem. An interesting feature, appearing in the present variational derivation, is a dual possibility concerning the tangential velocity on the boundary; it may be either the same as in irrotational flow (no condition) or zero, corresponding to the small-viscosity limit. The deeper meaning and the significance of these findings seem to deserve further analysis
Propagation of acoustic-gravity waves in inhomogeneous ocean environment based on modal expansions and HP-FEM
A coupled mode model is presented for the propagation of acoustic-gravity waves
in layered ocean waveguides. The analysis extends previous work for acoustic waves in
inhomogeneous environment. The coupled mode system is derived by means of a variational
principle in conjunction with local mode series expansion, obtained by utilizing eigenfunction
systems defined in the vertical section. These are obtained through the solution of vertical
eigenvalue problems formulated along the waveguide. A crucial factor is the inclusion of
additional modes accounting for the effects of spatialy varying boundaries and interfaces. This
enhancement provides an implicit summation for the slowly convergent part of the localmode
series, rendering the series rapidly convergent, increasing substantialy the efficiency of
the method. Particular aspects of the method include high order Lagrange Finite Element
Methods for the solution of local vertical eigenvalue problems in the case of multilayered
waveguides, and Gauss-type quadrature for the computation of the coupled-mode system
coefficients. The above aspects make the present method quite efficient for long range
propagation in extended waveguides, such as the ones found in geophysical applications, e.g.
ocean basins, as only few modes are needed for the accurate representation of the wave field
Young Researchers Advancing Computational Science: Perspectives of the Young Scientists Conference 2015
We present an annual international Young Scientists Conference (YSC) on computational science http://ysc.escience.ifmo.ru/, which brings together renowned experts and young researchers working in high-performance computing, data-driven modeling, and simulation of large-scale complex systems. The first YSC event was organized in 2012 by the University of Amsterdam, the Netherlands and ITMO University, Russia with the goal of opening a dialogue on the present and the future of computational science and its applications. We believe that the YSC conferences will strengthen the ties between young scientists in different countries, thus promoting future collaboration. In this paper we briefly introduce the challenges the millennial generation is facing; describe the YSC conference history and topics; and list the keynote speakers and program committee members. This volume of Procedia Computer Science presents selected papers from the 4th International Young Scientists Conference on Computational Science held on 25 June â 3 July 2015 in Athens, Greece