International audienceThe set of 3D inviscid primitive equations for the atmosphere is dimensionally reduced by a Discontinuous Galerkin discretization in one horizontal direction. The resulting model is a 2D system of balance laws where with a source term depending on the layering procedure and the choice of coupling fluxes, which is established in terms of upwind considerations. The "2.5D" system is discretized via a WENO-TVD scheme based in a flux limiter centered approach. We study four tests cases related to atmospheric phenomena to analyze the physical validity of the model
Six strategies to couple the dynamical core with physical parameterizations in atmospheric models ar...
The physical characteristics of mesoscale are analyzed, and results show that the unbalanced forced ...
The delta-Eddington approximation of Joseph, Wiscombe, and Weinman (1976) is extended to an atmosphe...
International audienceThe set of 3D inviscid primitive equations for the atmosphere is dimensionally...
Abstract. In this talk we present a new layered model for atmospheric applications. The model is der...
A two dimensional mesoscale atmospheric model is presented based on two systems of dynamical equatio...
AbstractAtmospheric flows of importance for weather forecasting are mostly characterized by a requir...
To meet the challenges posed by future generations of massively parallel supercomputers, a reformula...
To meet the challenges posed by future generations of massively parallel supercomputers a reformulat...
model, finite differences, accurate time-stepping. In this paper a 3-D model for pollutant transport...
Localized artificial viscosity stabilization of discontinuous Galerkin methods for nonhydrostatic me...
The physical characteristics of mesoscale are analyzed, and results show that the unbalanced forced ...
This project was targeting the development of a computational approach that would allow resolving cl...
A classic Discontinuous Galerkin Method with low-order polynomials and explicit as well as semi-impl...
In this chapter, we will derive the governing equations for a stratified inviscid atmosphere on an f...
Six strategies to couple the dynamical core with physical parameterizations in atmospheric models ar...
The physical characteristics of mesoscale are analyzed, and results show that the unbalanced forced ...
The delta-Eddington approximation of Joseph, Wiscombe, and Weinman (1976) is extended to an atmosphe...
International audienceThe set of 3D inviscid primitive equations for the atmosphere is dimensionally...
Abstract. In this talk we present a new layered model for atmospheric applications. The model is der...
A two dimensional mesoscale atmospheric model is presented based on two systems of dynamical equatio...
AbstractAtmospheric flows of importance for weather forecasting are mostly characterized by a requir...
To meet the challenges posed by future generations of massively parallel supercomputers, a reformula...
To meet the challenges posed by future generations of massively parallel supercomputers a reformulat...
model, finite differences, accurate time-stepping. In this paper a 3-D model for pollutant transport...
Localized artificial viscosity stabilization of discontinuous Galerkin methods for nonhydrostatic me...
The physical characteristics of mesoscale are analyzed, and results show that the unbalanced forced ...
This project was targeting the development of a computational approach that would allow resolving cl...
A classic Discontinuous Galerkin Method with low-order polynomials and explicit as well as semi-impl...
In this chapter, we will derive the governing equations for a stratified inviscid atmosphere on an f...
Six strategies to couple the dynamical core with physical parameterizations in atmospheric models ar...
The physical characteristics of mesoscale are analyzed, and results show that the unbalanced forced ...
The delta-Eddington approximation of Joseph, Wiscombe, and Weinman (1976) is extended to an atmosphe...