Does the Earth magnetic field spin up the polar vortex in the outer core?

Magnetic fields shield planetary surfaces, enabling life. Yet, the dynamo process producing Earth's magnetic field is still a mystery. Evidence suggests an intense polar vortex exists in Earth's liquid core, raising questions about its origin and role in the dynamo mechanism. This project explores the novel idea that Earth's magnetic field spins up this vortex, influencing the formation You will combine numerical simulations of magnetohydrodynamic (MHD) models with experiments using the Little Earth Experiment (LEE), a unique transparent model of Earth's core reproducing convective flows under Earth's rotation and magnetic effects. Work will occur in Coventry and at the high magnetic field laboratory in Grenoble, using some of the world's most powerful magnets. Expected Outcomes, Identify the regime where magnetic spin-up of the polar vortex occurs and determine its impact on generating the Earth’s dynamo. Gain expertise in geophysical fluid dynamics, numerical modelling, and experimental techniques while building an international scientific network. Why It Matters Understanding the dynamo process is vital to explaining planetary magnetic fields which protect life on Earth and other planets. This pioneering research could reveal new mechanisms powering Earth's magnetic shield, advancing planetary science and physics.

A minimum of a 2:1 first degree in a relevant discipline/subject area with at least 60% in the project element and 60% overall module average. Ability to engage in innovative research and complete PhD in 3.5 years. English proficiency with IELTS academic minimum 6.5 overall and 6.0 in each component.

Contact aa4111@coventry.ac.uk to learn more. Apply with full supporting documentation, a covering letter, and a 500-word statement showing relevance to the project.