Ramses Van der Toorn
Delft Institute of Applied Mathematics, Netherlands
R. (Ramses) van der Toorn (MSc in applied physics from Delft University of Technology) completed his PhD (cum laude, Utrecht University, 1997), on research in geophysical fluid dynamics, carried out atthe Netherlands Institute for Sea Research. He has since published and been active (including teaching,and serving conference committees as well asthe CMCinternational industrial standardization coalition) in semiconductor device physics and compact transistor modeling (from Philips Research Laboratories, and developing and hosting the world wide industrial standardMextram from Delft University of Technology). In parallel he has continued publishing scientific work in geophysical fluid dynamics. Dr. van der Toorn currently holds an assistant professor position, with a focus on research of applications of mathematics in geophysical fluid dynamics, at the Delft Institute of Applied Mathematics.
A comprehensive exposé will be presented covering the both intimate and elucidative interweavement of (differential) geometry and planetary fluid mechanics. It will be made explicit how coordinate-free representations of dynamics and representations with respect to chosen suitable coordinate systems are complementary, and how coordinate free representations are helpful to identify the role of geometrical objects in geophysical fluid dynamics (GFD). This will be presented both from the point of view of Eulerian fluid dynamics and from the point of view of a Lagrangian variational formulation. A slight generalization of Noether’s theorem then shows how the mathematical Lie group of rotations manifests itself in the mechanics of a fluid shell covering a rotating planet in the guise ofglobal planetary angular momentum dynamics. The underlying approximate spherical symmetry of the geopotential will be thorougly discussed. As an illustration, the application of the theory to the dynamics underlying trajectories of oceanic monopolar vortices, including their intrinsic westward drift, on a rotating sphere, will be outlined.
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