
Gonzalo Gonzalez De Diego
University of Oxford
Andrew Wiles Building
Radcliffe Observatory Quarter
Woodstock Road
Oxford
OX2 6GG
On the finite element approximation of a semicoercive Stokes variational inequality arising in glaciology. Gonzalo G. de Diego, Patrick E. Farrell, Ian J. Hewitt, SIAM Journal on Numerical Analysis 61 (1), 1-25 (2023)
Numerical approximation of viscous contact problems applied to glacial sliding. Gonzalo G. de Diego, Patrick E. Farrell, Ian J. Hewitt, Journal of Fluid Mechanics, 938 A21 (2022)
Convergence analysis of the scaled boundary finite element method for the Laplace equation. Bertrand, F; Boffi, D; de Diego, G, Advances in Computational Mathematics, Volume 47, Article number 34 (2021)
Inclusion of no-slip boundary conditions in the MEEVC scheme. de Diego, G; Palha, A; Gerritsma, M. Journal of Computational Physics, Volume 378, pp. 615-633 (2019)
I am interested in the development of numerical methods for studying glaciers and ice sheets to help us comprehend their dynamics and their role in our climate system. My PhD research has focused on viscous contact problems, in which a viscous fluid slides on a solid surface from which it can detach and reattach. Since ice is usually modelled as a viscous fluid with a nonlinear rheology, such problems arise in glaciology. One example is that of a marine ice sheet, which slides from the continent and into the ocean, where it goes afloat at the grounding line. Given that large areas of the West Antarctica are floating ice shelves, the dynamics of grounding lines are extremely important for understanding how these masses of ice will evolve in our changing climate.
MT19: TA for B6.1 Numerical Solution of Differential Equations I
HT20: TA for C6.4 Finite Element Method for PDEs
MT 20: Tutor for Numerical Solution of Differential Equations I, MSc in Mathematical Modelling and Scientific Computing
MT 20, HT 21, TT 21: College Tutor for Prelims Analysis I-III
HT22: Tutor for C6.4 Finite Element Method for PDEs