Imperial College London

ProfessorDavidHam

Faculty of Natural SciencesDepartment of Mathematics

Professor of Computational Mathematics
 
 
 
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Contact

 

+44 (0)20 7594 5003david.ham Website CV

 
 
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Location

 

753Huxley BuildingSouth Kensington Campus

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Summary

 

Publications

Citation

BibTex format

@article{Kärnä:2018:10.5194/gmd-2017-292,
author = {Kärnä, T and Kramer, SC and Mitchell, L and Ham, DA and Piggott, MD and Baptista, AM},
doi = {10.5194/gmd-2017-292},
journal = {Geoscientific Model Development},
pages = {4359--4382},
title = {Thetis coastal ocean model: discontinuous Galerkin discretization for the three-dimensional hydrostatic equations},
url = {http://dx.doi.org/10.5194/gmd-2017-292},
volume = {11},
year = {2018}
}

RIS format (EndNote, RefMan)

TY  - JOUR
AB - Unstructured grid ocean models are advantageous for simulating the coastal ocean and river-estuary-plume systems. However, unstructured grid models tend to be diffusive and/or computationally expensive which limits their applicability to real life problems. In this paper, we describe a novel discontinuous Galerkin (DG) finite element discretization for the hydrostatic equations. The formulation is fully conservative and second-order accurate in space and time. Monotonicity of the advection scheme is ensured by using a strong stability preserving time integration method and slope limiters. Compared to previous DG models advantages include a more accurate mode splitting method, revised viscosity formulation, and new second-order time integration scheme. We demonstrate that the model is capable of simulating baroclinic flows in the eddying regime with a suite of test cases. Numerical dissipation is well-controlled, being comparable or lower than in existing state-of-the-art structured grid models.
AU - Kärnä,T
AU - Kramer,SC
AU - Mitchell,L
AU - Ham,DA
AU - Piggott,MD
AU - Baptista,AM
DO - 10.5194/gmd-2017-292
EP - 4382
PY - 2018///
SN - 1991-959X
SP - 4359
TI - Thetis coastal ocean model: discontinuous Galerkin discretization for the three-dimensional hydrostatic equations
T2 - Geoscientific Model Development
UR - http://dx.doi.org/10.5194/gmd-2017-292
UR - http://hdl.handle.net/10044/1/54780
VL - 11
ER -