Incorporating multiscale mechanics in lithium-ion battery models
Giudici, A Galvis, A Sahu, S Timms, R Please, C Chapman, J Foster, J (20 Aug 2026)
A transform approach to the supercooled Stefan problem
Hambly, B Blore, T Electronic Communications in Probability
A likelihood-based framework for simultaneously learning both noise and growth dynamics using biologically-informed neural networks
Crossley, R Baker, R Bulletin of Mathematical Biology
Multilevel lattice-based kernel approximation for elliptic PDEs with random coefficients
Giles, M Gilbert, A Kuo, F Sloan, I Srikumar, A Numerische Mathematik
Thu, 03 Dec 2026

12:00 - 13:00
L3

TBC

Dr. Mazi Jalaal
(DAMTP, University of Cambridge)

The join button will be shown 30 minutes before the seminar starts.

Thu, 26 Nov 2026

12:00 - 13:00
L3

TBC

Dr Helen Walker
(UK Battery Industrialisation Centre)

The join button will be shown 30 minutes before the seminar starts.

Thu, 19 Nov 2026

12:00 - 13:00
L3

DPhil Talks

Orson Hart, Maria Reboredo Prado, Chun Lam Li, Vedanta Thapar
((Mathematical Institute University of Oxford))

The join button will be shown 30 minutes before the seminar starts.

Abstract

Maria Reboredo Prado


Stratosphere-Troposphere Interactions: Understanding how the Upper Atmosphere Shapes the Weather and Climate We See.
Abstract: 
It is well known that the stratosphere – the second layer of the atmosphere – can exert a powerful influence on weather and climate at the surface. This influence is particularly important in winter, when the strength of the stratospheric polar vortex — a belt of fast-moving winds encircling the pole — can vary dramatically. If the impacts of these variations on the lower atmosphere were better understood and more accurately represented in forecast models, they could provide early signals of winter weather patterns, improving predictions on subseasonal to seasonal timescales. Yet, the mechanisms by which changes high in the atmosphere produce a response near the surface remain poorly understood. 
In this talk, I will use an idealised atmospheric model to test how much of this downward effect can be explained by large-scale balanced dynamics. The model allows individual processes – such as atmospheric cooling, surface friction, and boundary effects – to be switched on or off, making it possible to assess their relative roles in shaping the surface response. A key improvement on previous theoretical models is that the displacement of the tropopause — the boundary between the troposphere and stratosphere – emerges naturally as part of the flow’s response to forcing. Overall, this framework provides a controlled setting for identifying the dynamical mechanisms that transmit stratospheric disturbances to the surface.

 

Orson Hart, Chun Lam Li, Vedanta Thapar

Thu, 12 Nov 2026

12:00 - 13:00
L3

TBC

Dr Kasia Warburton
(School of Mathematics, University of Bristol)

The join button will be shown 30 minutes before the seminar starts.

Further Information

Kasia Warburton works on understanding the flow of glaciers and ice sheets (Antarctica and Greenland) using fluid dynamics. She studies the flow of water and sediment underneath the ice that control how fast the ice moves.

Thu, 05 Nov 2026

12:00 - 13:00
L3

TBC

Dr Alexandra Tzella
(Department of Mathematics University of Birmingham)

The join button will be shown 30 minutes before the seminar starts.

Thu, 29 Oct 2026

12:00 - 13:00
L3

Opinion Dynamics on Networks

Prof. Mason Porter
(University of California, Los Angeles)

The join button will be shown 30 minutes before the seminar starts.

Abstract

In mathematical models of opinion dynamics, individuals interact with each other and adjust their opinions based on their interactions. In opinion models, network structures determine which individuals can interact with each other and thereby affect how opinions change with time. In this talk, I will introduce opinion models and why scientists study them. I will also discuss several variants of bounded-confidence models (BCMs), in which opinions take continuous values in a region, and I will examine how network structure affects the formation of consensus, polarization, and fragmentation of populations.

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