We describe FESOM-C, the coastal branch of the Finite-volumE Sea ice – Ocean Model (FESOM2), which shares with FESOM2 many numerical aspects, in particular its finite-volume cell-vertex discretization. Its dynamical core differs in the implementation of time stepping, the use of a terrain-following vertical coordinate, and the formulation for hybrid meshes composed of triangles and quads. The first two distinctions were critical for coding FESOM-C as an independent branch. The hybrid mesh capability improves numerical efficiency, since quadrilateral cells have fewer edges than triangular cells. They do not suffer from spurious inertial modes of the triangular cell-vertex discretization and need less dissipation. The hybrid mesh capability a...
We analyze obvious and less obvious advantages/difficulties,including relative numeric efficiency, o...
Numerical modeling is now, along with experiment and theory, part of the scientific method. Numerica...
To circumvent the problems which arise at the discretizing stage of ocean general circulation models...
We describe FESOM-C, the coastal branch of the Finite-volumE Sea ice -- Ocean Model (FESOM2), which ...
Abstract. Version 2 of the unstructured-mesh Finite-Element Sea ice–Ocean circulation Model (FESOM) ...
FESOM2.0 builds on the framework of its predecessor, FESOM1.4, using its sea ice component Finite-El...
A newly developed coastal model, FESOM-C, based on three-dimensional unstructured meshes and finite ...
Unstructured meshes are common in coastal modeling, but still rarely used for modeling the large-sca...
Unstructured meshes offer geometric flexibility. In the context of large-scale ocean modeling they ...
Unstructured-mesh models are common in coastal ocean modeling, but their applications are still at t...
We discuss the performance of the Finite Element Ocean Model (FESOM) on locally eddy-resolving globa...
The Finite Element Sea Ice-Ocean Model (FESOM) is the first global ocean general circulation model b...
There is a growing need in the high quality estimations of long-term dynamics and circulation featur...
Abstract. Computation of barotropic and meridional overturning streamfunctions for models formulated...
Numerical modelling of coastal zone dynamics provides basis for solving a wide range of hydrogeolog...
We analyze obvious and less obvious advantages/difficulties,including relative numeric efficiency, o...
Numerical modeling is now, along with experiment and theory, part of the scientific method. Numerica...
To circumvent the problems which arise at the discretizing stage of ocean general circulation models...
We describe FESOM-C, the coastal branch of the Finite-volumE Sea ice -- Ocean Model (FESOM2), which ...
Abstract. Version 2 of the unstructured-mesh Finite-Element Sea ice–Ocean circulation Model (FESOM) ...
FESOM2.0 builds on the framework of its predecessor, FESOM1.4, using its sea ice component Finite-El...
A newly developed coastal model, FESOM-C, based on three-dimensional unstructured meshes and finite ...
Unstructured meshes are common in coastal modeling, but still rarely used for modeling the large-sca...
Unstructured meshes offer geometric flexibility. In the context of large-scale ocean modeling they ...
Unstructured-mesh models are common in coastal ocean modeling, but their applications are still at t...
We discuss the performance of the Finite Element Ocean Model (FESOM) on locally eddy-resolving globa...
The Finite Element Sea Ice-Ocean Model (FESOM) is the first global ocean general circulation model b...
There is a growing need in the high quality estimations of long-term dynamics and circulation featur...
Abstract. Computation of barotropic and meridional overturning streamfunctions for models formulated...
Numerical modelling of coastal zone dynamics provides basis for solving a wide range of hydrogeolog...
We analyze obvious and less obvious advantages/difficulties,including relative numeric efficiency, o...
Numerical modeling is now, along with experiment and theory, part of the scientific method. Numerica...
To circumvent the problems which arise at the discretizing stage of ocean general circulation models...