In this work, the fully compressible, three-dimensional, nonhydrostatic atmospheric model called All Scale Atmospheric Model (ASAM) is presented. A cut cell approach is used to include obstacles and orography into the Cartesian grid. Discretization is realized by a mixture of finite differences and finite volumes and a state limiting is applied. Necessary shifting and interpolation techniques are outlined. The method can be generalized to any other orthogonal grids, e.g., a lat–long grid. A linear implicit Rosenbrock time integration scheme ensures numerical stability in the presence of fast sound waves and around small cells. Analyses of five two-dimensional benchmark test cases from the literature are carried out to show that the describe...
Several tests of a model with a cut-cell representation of orography are presented: a resting atmosp...
The formulation of a fully compressible nonhydrostatic atmospheric model called the Model for Predic...
Physical processes in the atmosphere develop on a wide range of spatial and temporal scales. Meteoro...
In this work, the fully compressible, three-dimensional, nonhydrostatic atmospheric model called A...
Moves to increasingly high-resolution models give rise to more variations in the underlying orograph...
Numerical weather and climate models are using increasingly fine meshes that resolve small-scale, s...
Studies of the small-scale atmosphere improve our understanding of dynamics and interactions that oc...
Cut-cell meshes present an attractive alternative to terrain-following coordinates for the represent...
International audienceA modified version of an operational 3-D, non-hydrostatic, limited-area atmosp...
We introduce a second-order numerical scheme for compressible atmospheric motions at small to planet...
Correct representation of physical processes, the parametrizations, and their interaction with the r...
A three-dimensional semi-implicit edge-based unstructured-mesh model is developed that integrates no...
The paper advances the limited-area anelastic model (Smolarkiewicz et al. (2013) [45]) for investiga...
In this thesis, we study next generation techniques for the numerical simulation of global atmospher...
The formulation of a fully compressible nonhydrostatic atmospheric model called theModel for Predict...
Several tests of a model with a cut-cell representation of orography are presented: a resting atmosp...
The formulation of a fully compressible nonhydrostatic atmospheric model called the Model for Predic...
Physical processes in the atmosphere develop on a wide range of spatial and temporal scales. Meteoro...
In this work, the fully compressible, three-dimensional, nonhydrostatic atmospheric model called A...
Moves to increasingly high-resolution models give rise to more variations in the underlying orograph...
Numerical weather and climate models are using increasingly fine meshes that resolve small-scale, s...
Studies of the small-scale atmosphere improve our understanding of dynamics and interactions that oc...
Cut-cell meshes present an attractive alternative to terrain-following coordinates for the represent...
International audienceA modified version of an operational 3-D, non-hydrostatic, limited-area atmosp...
We introduce a second-order numerical scheme for compressible atmospheric motions at small to planet...
Correct representation of physical processes, the parametrizations, and their interaction with the r...
A three-dimensional semi-implicit edge-based unstructured-mesh model is developed that integrates no...
The paper advances the limited-area anelastic model (Smolarkiewicz et al. (2013) [45]) for investiga...
In this thesis, we study next generation techniques for the numerical simulation of global atmospher...
The formulation of a fully compressible nonhydrostatic atmospheric model called theModel for Predict...
Several tests of a model with a cut-cell representation of orography are presented: a resting atmosp...
The formulation of a fully compressible nonhydrostatic atmospheric model called the Model for Predic...
Physical processes in the atmosphere develop on a wide range of spatial and temporal scales. Meteoro...