AbstractVertical discretization of the hydrostatic atmospheric models is considered. The matrices of the vertical structure are derived for three different vertical approximations: simplified vertical discretization, Charney-Phillips and Lorenz staggered grids. Analysis of the properties of these vertical structure matrices is performed using matrix factorization and results about total positivity. The well-posedness of initial value problem for vertically discretized equations is shown based on oscillatory properties of the vertical structure matrices
The article of record as published may be found at http://dx.doi.org/10.5194/gmd-7-2717-2014The non-...
Six strategies to couple the dynamical core with physical parameterizations in atmospheric models ar...
The article of record as published may be found at http://dx.doi.org/10.5194/gmdd-7-4119-2014Discuss...
AbstractVertical discretization of the hydrostatic atmospheric models is considered. The matrices of...
AbstractHydrostatic atmospheric models in a generalized vertical coordinate are considered. The gove...
Accurate representation of different kinds of wave motion is essential for numerical models of the a...
This work is a first step in the direction of implementing a high-order finite-element discretizatio...
An entirely new type of equation for forecasting atmospheric parameters is derived by applying varia...
This thesis demonstrates a new non-staggered-grid finite-volume method for dynamical cores in atmosp...
The vertical grid of an atmospheric model assigns dynamic and thermo- dynamic variables to grid loca...
Abstract:- The linear stability of the semi-implicit primitive equation models with a central finite...
Atmospheric modeling systems require economical methods to solve the non-hydrostatic Euler equations...
The finite-element method with B splines is used for definition of vertical operators in the nonhydr...
The article of record as published may be found at http://dx.doi.org/10.5194/gmdd-7-3717-2014Discuss...
International audienceThe set of 3D inviscid primitive equations for the atmosphere is dimensionally...
The article of record as published may be found at http://dx.doi.org/10.5194/gmd-7-2717-2014The non-...
Six strategies to couple the dynamical core with physical parameterizations in atmospheric models ar...
The article of record as published may be found at http://dx.doi.org/10.5194/gmdd-7-4119-2014Discuss...
AbstractVertical discretization of the hydrostatic atmospheric models is considered. The matrices of...
AbstractHydrostatic atmospheric models in a generalized vertical coordinate are considered. The gove...
Accurate representation of different kinds of wave motion is essential for numerical models of the a...
This work is a first step in the direction of implementing a high-order finite-element discretizatio...
An entirely new type of equation for forecasting atmospheric parameters is derived by applying varia...
This thesis demonstrates a new non-staggered-grid finite-volume method for dynamical cores in atmosp...
The vertical grid of an atmospheric model assigns dynamic and thermo- dynamic variables to grid loca...
Abstract:- The linear stability of the semi-implicit primitive equation models with a central finite...
Atmospheric modeling systems require economical methods to solve the non-hydrostatic Euler equations...
The finite-element method with B splines is used for definition of vertical operators in the nonhydr...
The article of record as published may be found at http://dx.doi.org/10.5194/gmdd-7-3717-2014Discuss...
International audienceThe set of 3D inviscid primitive equations for the atmosphere is dimensionally...
The article of record as published may be found at http://dx.doi.org/10.5194/gmd-7-2717-2014The non-...
Six strategies to couple the dynamical core with physical parameterizations in atmospheric models ar...
The article of record as published may be found at http://dx.doi.org/10.5194/gmdd-7-4119-2014Discuss...