A finite element discretization of the streamfunction formulation of the stationary quasi-geostrophic equations of the ocean EL Foster, T Iliescu, Z Wang Computer Methods in Applied Mechanics and Engineering 261, 105-117, 2013 | 43 | 2013 |
Clipping simple polygons with degenerate intersections EL Foster, K Hormann, RT Popa Computers & Graphics: X 2, 100007, 2019 | 18 | 2019 |
A structure preserving scheme for the Kolmogorov–Fokker–Planck equation EL Foster, J Lohéac, MB Tran Journal of Computational Physics 330, 319-339, 2017 | 18 | 2017 |
A two-level finite element discretization of the streamfunction formulation of the stationary quasi-geostrophic equations of the ocean EL Foster, T Iliescu, DR Wells Computers & Mathematics with Applications 66 (7), 1261-1271, 2013 | 13 | 2013 |
Finite Elements for the quasi-geostrophic equations of the ocean EL Foster Virginia Tech, 2013 | 8 | 2013 |
A conforming finite element discretization of the streamfunction form of the unsteady quasi-geostrophic equations EL Foster, T Iliescu, DR Wells arXiv preprint arXiv:1405.7836, 2014 | 5 | 2014 |
Clipping of arbitrary polygons with degeneracies EL Foster, JR Overfelt arXiv preprint arXiv:1211.3376, 2012 | 3 | 2012 |
Multicore and manycore: Hybrid computing architectures and applications P Valero-Lara, A Paz-Gallardo, EL Foster, M Prieto-Matías, A Pinelli, ... Innovative Research and Applications in Next-Generation High Performance …, 2016 | 2 | 2016 |
Model Comparison for Abiotic versus Biotic Pollen Dispersal. EL Foster, DM Chan, D Rodney J. Nonlinear Dynamics Psychol Life Sci. 20 (4), 471-83, 2016 | 1 | 2016 |
An agent based gene flow model E Foster Virginia Commonwealth University, 2009 | 1 | 2009 |
Large Eddy Simulation of the Quasi-Geostrophic Equations of Oceanic Flows T Iliescu, O San, Z Wang, E Foster, A Staples AGU Fall Meeting Abstracts 2012, NG51D-1791, 2012 | | 2012 |
A Finite Element Solution to the Pure Stream Function Form of the Stationary Quasi-Geostophic Flow Equations EL Foster Southeastern Atlantic Regional Conference on Differential Equations, 0 | | |