I am a PhD student studying physical oceanography at the University of Oxford. I am based at the department of Atmospheric, Oceanic and Planetary Physics (AOPP) and a student of the Environmental Research DTP.
I take an interest in the fluid dynamics of the ocean circulation. I study the dynamics of ocean gyres and how they are influenced by both mesoscale eddies and interactions with the sea floor. I design idealized models, develop diagnostic methods, and use pen-and-paper analysis to find minimal descriptions of ocean processes seen in models and observations.
My current research project is a collaboration between the University of Oxford and the Met Office.
DPhil (Phd) in Physical Oceanography, 2019-
University of Oxford
MPhys in Physics, 2015-2019
University of Oxford
Gyres are prominent surface structures in the global ocean circulation that often interact with the sea floor in a complex manner. Diagnostic methods, such as the depth-integrated vorticity budget, are needed to assess exactly how such model circulations interact with the bathymetry. Terms in the vorticity budget can be integrated over the area enclosed by streamlines to identify forces that spin gyres up and down. In this article we diagnose the depth-integrated vorticity budgets of both idealized gyres and the Weddell Gyre in a realistic global model. It is shown that spurious forces play a significant role in the dynamics of all gyres presented and that they are a direct consequence of the Arakawa C-grid discretization and the z-coordinate representation of the sea floor. The spurious forces include a numerical beta effect and interactions with the sea floor which originate from the discrete Coriolis force when calculated with the following schemes: the energy conserving scheme; the enstrophy conserving scheme; and the energy and enstrophy conserving scheme. Previous studies have shown that bottom pressure torques provide the main interaction between the depth-integrated flow and the sea floor. Bottom pressure torques are significant, but spurious interactions with bottom topography are similar in size. Possible methods for reducing the identified spurious topographic forces are discussed. Spurious topographic forces can be alleviated by using either a B-grid in the horizontal plane or a terrain-following vertical coordinate.