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Solving incompressible flow problems with parallel spectral element methods
Parallel spectral element models are built for the Navier-Stokes equations and the shallow water equations with nonstaggered grid formulations. The optimized computational efficiency of these parallel spectral element models comes not only from the exponential convergence of their numerical solutions, but also from their efficient usage of the powerful vector-processing units of the latest parallel architectures. Furthermore, the communication cost of the spectral element model is lower than that of the h-type finite element model, partly because many fewer redundant nodal values have to be stored. The nonstaggered grid formulations perform well in iterative procedures which are highly in parallel. Implementations of these models are carried out on the Connection Machine systems. The present work shows that the high-order domain decomposition methods can be efficiently applied in a data parallel programming environment
FullSWOF_Paral: Comparison of two parallelization strategies (MPI and SKELGIS) on a software designed for hydrology applications
In this paper, we perform a comparison of two approaches for the
parallelization of an existing, free software, FullSWOF 2D (http://www.
univ-orleans.fr/mapmo/soft/FullSWOF/ that solves shallow water equations for
applications in hydrology) based on a domain decomposition strategy. The first
approach is based on the classical MPI library while the second approach uses
Parallel Algorithmic Skeletons and more precisely a library named SkelGIS
(Skeletons for Geographical Information Systems). The first results presented
in this article show that the two approaches are similar in terms of
performance and scalability. The two implementation strategies are however very
different and we discuss the advantages of each one.Comment: 27 page
Spectral/hp element methods: recent developments, applications, and perspectives
The spectral/hp element method combines the geometric flexibility of the
classical h-type finite element technique with the desirable numerical
properties of spectral methods, employing high-degree piecewise polynomial
basis functions on coarse finite element-type meshes. The spatial approximation
is based upon orthogonal polynomials, such as Legendre or Chebychev
polynomials, modified to accommodate C0-continuous expansions. Computationally
and theoretically, by increasing the polynomial order p, high-precision
solutions and fast convergence can be obtained and, in particular, under
certain regularity assumptions an exponential reduction in approximation error
between numerical and exact solutions can be achieved. This method has now been
applied in many simulation studies of both fundamental and practical
engineering flows. This paper briefly describes the formulation of the
spectral/hp element method and provides an overview of its application to
computational fluid dynamics. In particular, it focuses on the use the
spectral/hp element method in transitional flows and ocean engineering.
Finally, some of the major challenges to be overcome in order to use the
spectral/hp element method in more complex science and engineering applications
are discussed
Mixed finite elements for numerical weather prediction
We show how two-dimensional mixed finite element methods that satisfy the
conditions of finite element exterior calculus can be used for the horizontal
discretisation of dynamical cores for numerical weather prediction on
pseudo-uniform grids. This family of mixed finite element methods can be
thought of in the numerical weather prediction context as a generalisation of
the popular polygonal C-grid finite difference methods. There are a few major
advantages: the mixed finite element methods do not require an orthogonal grid,
and they allow a degree of flexibility that can be exploited to ensure an
appropriate ratio between the velocity and pressure degrees of freedom so as to
avoid spurious mode branches in the numerical dispersion relation. These
methods preserve several properties of the C-grid method when applied to linear
barotropic wave propagation, namely: a) energy conservation, b) mass
conservation, c) no spurious pressure modes, and d) steady geostrophic modes on
the -plane. We explain how these properties are preserved, and describe two
examples that can be used on pseudo-uniform grids: the recently-developed
modified RT0-Q0 element pair on quadrilaterals and the BDFM1-\pdg element pair
on triangles. All of these mixed finite element methods have an exact 2:1 ratio
of velocity degrees of freedom to pressure degrees of freedom. Finally we
illustrate the properties with some numerical examples.Comment: Revision after referee comment
Compatible finite element spaces for geophysical fluid dynamics
Compatible finite elements provide a framework for preserving important structures in equations of geophysical uid dynamics, and are becoming important in their use for building atmosphere and ocean models. We survey the application of compatible finite element spaces to geophysical uid dynamics, including the application to the nonlinear rotating shallow water equations, and the three-dimensional compressible Euler equations. We summarise analytic results about dispersion relations and conservation properties, and present new results on approximation properties in three dimensions on the sphere, and on hydrostatic balance properties
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