Performance Pitfalls in the Dune Grid Interface

3D Benchmark on Discretization Schemes for Anisotropic Diffusion Problems on General Grids

Benchmark 3D: The Compact Discontinuous Galerkin 2 Scheme

Compact and Stable Discontinuous Galerkin Methods with Application to Atmospheric Flows

CDG Method for Navier-Stokes Equations

Simulation of Geophysical Problems with DUNE-FEM

Stabilization for Discontinuous Galerkin Methods Applied to Systems of Conservation Laws

Higher Order Adaptive and Parallel Simulations Including Dynamic Load Balancing with the Software Package DUNE

The compact discontinuous Galerkin method for elliptic problems

Parallel Adaptive Simulation of PEM Fuel Cells

The Distributed and Unified Numerics Environment (DUNE)

A general object oriented framework for discretizing non-linear evolution equations

An efficient implementation of an adaptive and parallel grid in DUNE

Towards a Unified Framework for Scientific Computing

A dynamic two-phase flow model of proton exchange membrane fuel cells

Advances in DUNE

Finite Volumes for Complex Applications IX : Methods, Theoretical Aspects, Examples

Carbon exchange in boreal ecosystems: upscaling and the impacts of natural disturbances

Boreal forests and peatlands are globally significant carbon stores but they are threatened by rising air temperatures and changes in precipitation regimes and the frequency of natural disturbances. Predicting how the boreal biome will respond to climate change depends on being able to accurately model and upscale the greenhouse gas fluxes between these ecosystems and the atmosphere. This thesis f

Denitrification by benthic foraminifera and their contribution to N-loss from a fjord environment

Oxygen and nitrate availabilities impact the marine nitrogen cycle at a range of spatial and temporal scales. Here, we demonstrate the impact of denitrifying foraminifera on the nitrogen cycle at two oxygen and nitrate contrasting stations in a fjord environment (Gullmar Fjord, Sweden). Denitrification by benthic foraminifera was determined through the combination of specific density counting per

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