2021
DOI: 10.1080/16000870.2021.1876341
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Coastal ocean forecasting on the GPU using a two-dimensional finite-volume scheme

Abstract: In this work, we take a modern high-resolution finite-volume scheme for solving the rotational shallowwater equations and extend it with features required to run real-world ocean simulations. Our contributions include a spatially varying north vector and Coriolis term required for large scale domains, moving wet-dry fronts, a static land mask, bottom shear stress, wind forcing, boundary conditions for nesting in a global model, and an efficient model reformulation that makes it well-suited for massively parall… Show more

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Cited by 6 publications
(9 citation statements)
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References 35 publications
(39 reference statements)
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“…The model error for hu$$ hu $$ and hv$$ hv $$ is then inferred according to geostrophic balance to ensure physical feasibility. Further details about this model are available in Brodtkorb and Holm (2021) and Holm et al (2020).…”
Section: Comparison For Drift Trajectory Forecasting In a Simplified ...mentioning
confidence: 99%
“…The model error for hu$$ hu $$ and hv$$ hv $$ is then inferred according to geostrophic balance to ensure physical feasibility. Further details about this model are available in Brodtkorb and Holm (2021) and Holm et al (2020).…”
Section: Comparison For Drift Trajectory Forecasting In a Simplified ...mentioning
confidence: 99%
“…The model error for hu and hv is then inferred according to geostrophic balance to ensure physical feasibility. Further details about this model are available in Brodtkorb and Holm (2021) and Holm et al (2020).…”
Section: Simplified Ocean Modelmentioning
confidence: 99%
“…Values for K j,k and L j,k are obtained by evaluating the integrals in ( 4) by a recursive sum starting from zero at the boundary. Note that the recursive sums for K and L mostly cancel in the reconstruction and are reduced to local operations [1,Sect. 3.1].…”
Section: Well-balanced Schemementioning
confidence: 99%
“…Finally, we study the consequence of using different flux terms and slope limiters when using the CDKLM scheme for simulating a real-world oceanographic scenario. Here, we utilize the full GPUaccelerated framework from [1], in which land mask, bathymetry, initial and boundary conditions, domain orientation, and wind forcing are taken from the operational model NorKyst800 [9], with 800 m horizontal resolution. Figure 5 shows water velocity at 23 h for a few selected values of ϕ and θ for CDKLM.…”
Section: Numerical Experimentsmentioning
confidence: 99%
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